{'fraction_non_alphanumeric': 0.031808986795368026, 'fraction_numerical': 0.022347525525238526, 'mean_word_length': 4.72306289881495, 'pattern_counts': {'":': 0, '<': 15, '<?xml version=': 0, '>': 4, 'https://': 0, 'lorem ipsum': 0, 'www.': 0, 'xml': 0}, 'pii_count': 0, 'substrings_counts': 0, 'word_list_counts': {'cursed_substrings.json': 3, 'profanity_word_list.json': 0, 'sexual_word_list.json': 0, 'zh_pornsignals.json': 0}}
Evaluating Strategies to Improve Water Availability and Lateral Root Growth of Plants Grown in the Rice-Growing Lowlands of the Lower Mekong Basin

: Overcoming constraints that poorly structured lowland rice-growing soils of the Lower Mekong River Basin present for growing non-rice crops during the dry season would have a signiﬁcant positive impact on the livelihood of smallholder farmers. This study investigated whether the use of soil organic amendments, bed architecture (conventional, ﬂat and narrow) and water application methods (sprinkler, furrow and over-bed irrigation) could improve plant water availability in typical rice-growing soils of Cambodia and Laos by either improving the movement of water into beds or the growth of the root system. Five experiments were conducted over two dry seasons on peanut and maize grown in a bed/furrow system. Organic amendments assessed were rice straw, cow/goat manure, biochar, manure plus rice straw and biochar plus manure. Results showed that compared with conventional bed/furrow design, narrowing beds increased soil moisture availability for peanut, whilst higher grain yield and water productivity were achieved with sprinkler irrigation than furrow irrigation. Placing a layer of sub-surface straw within beds did not consistently enhance soil moisture or improve root development. The study showed that maize grown on soil amended with biochar plus cow manure under a furrow irrigation system and on rice straw under sprinkler irrigation produced yields above the average yield that models have simulated for maize grown on these soils. These ﬁndings present opportunities to enhance maize production on lowland soils across Cambodia and Laos. The contrary was observed for peanut production, which indicates that factors other than water might be detrimentally affecting crop yields.


Introduction
It is estimated that agriculture provides livelihoods for approximately 60% of the population in the Lower Mekong River Basin (LMB) [1]. The LMB covers land of four south east Asian nations, Thailand, Laos, Cambodia and Vietnam, and is currently home to approximately 60 million people. Some 75-85% of the people from these countries are rural-based, poor and depend directly on water for food [2]. Among the countries through which the Mekong River passes, Cambodia and Laos have been identified by the United Nations World Food Programme as two of the most impoverished nations in southeast Asia, with high rates of poverty, food insecurity and poor nutrition, particularly amongst small landholders. Due to the tropical climate that characterizes the LMB with annual wet (>2000 mm) and dry cycles, smallholder production of rain-fed rice is the main agricultural activity in this region. Most of the rice production area (80%) is concentrated in the lowlands of the LMB where there are limited opportunities for growing alternative crops to rice, particularly during the wet season.
Incorporation of higher value non-rice crops during the dry season in rotation with rice has the potential to significantly improve income, water productivity, human nutrition and food security in the lowland production systems [3]. The incorporation of these crops into the rotations of smallholder farms, along with increasing the agricultural production across the region, could be an important pathway for improving average household income and general standards of living.
Research aimed at investigating the productivity of dry-season crops in both Cambodia and Laos has indicated that these systems are subject to major production constraints, including drought and low soil fertility [3]. Lowland soils are typically sandy in texture and prone to hard setting, lacking in both organic matter and cation exchange capacity (CEC), acidic in the aerobic state and containing high levels of aluminum, particularly in the subsoil [4,5]. Recently, Ballester et al. [6] highlighted the poor lateral movement of water in these soils, which leads to inadequate refilling of the root zone, a particular limitation for the establishment of furrow-irrigated dry-season crop production in the region.
The use of soil organic amendments may enhance soil structure and increase its water holding capacity and fertility, particularly during the first season of amendment [7]. Research conducted in long-term experiments has shown that regular addition of organic amendment improves soil fertility and structural stability, enhances total organic N levels and reduces bulk density [8]. Addition of woody and other organic amendments have also shown potential to improve water holding capacity of soils [9]. The use of readily available and low-cost amendments such as rice husk biochar or manure compost has been proposed to enhance soil properties and increase agricultural productivity [10,11]. For example, research conducted by Mekuria et al. [12] on Acrisol soils showed that the use of organic and clay-based soil amendments increased soil properties and maize production in central Laos.
For dry-season crop production under bed/furrow systems, soil organic interventions could increase root access to water by either improving the lateral movement of water into beds or promoting the lateral expansion of roots that are otherwise limited in such compacted and physically strong soils. The main objective of this study was to use a set of experiments conducted over two dry seasons on typical rice-growing soils of the lowlands of Cambodia and Laos to investigate the effect of soil organic interventions, bed architecture and water application methods on water availability, belowground and aboveground biomass production and yield of peanut and maize. The experiments were conducted on maize (Zea mays Linnaeus) in Cambodia and peanut (Arachis hypogaea Linnaeus) in Laos, which are two of the major non-rice crops grown in these countries [13]. Using agronomic management, the lateral water movement constraint reported in Ballester et al. [6] may be overcome, which would provide major impact across large areas of south east Asia for increased dry season non-rice crop yields.  (Figure 1). More details about the location of the sites can be found in Ballester et al. (2019). Soil at these locations was a typical lowland rice-growing soil classified as Gleyic Acrisol based on the FAO/UNESCO classification [14]. At both sites, soil at 0-40 cm depth was predominantly sandy loam (62.0% sand and 27.0% silt at CARDI, and 58.8% sand and 29.6% silt at PNG) with the presence of clay (~20%) increasing in the 40-60 cm soil layer. At CARDI, soil pH in 2016 pre-planting was 6.72 and 7.12 at 0-20 cm and 20-50 cm depth, respectively. At PNG, soil pH in 2016 pre-land preparation was 5.36 at 0-20 cm depth and averaged 5.91 in the 20-60 cm soil layer. More details regarding the physico-chemical properties of the soils at both sites can be found in Table 2 in Ballester et al. [6].

Study Site Locations
The study was conducted during the 2016/17 and 2017/18 dry seasons (from December to April) at the Phone Ngam Rice Research Centre, PNG (15°08′14.97" N, 105°47′13.78" E elevation 101 m), Pakse district, Champasak province in southern Laos and the Cambodian Agricultural Research and Development Institute, CARDI (11°28′34.27" N, 104°48′32.26" E elevation 17 m) Kambol district, Phnom Penh city in Cambodia (Figure 1). More details about the location of the sites can be found in Ballester et al. (2019). Soil at these locations was a typical lowland rice-growing soil classified as Gleyic Acrisol based on the FAO/UNESCO classification [14]. At both sites, soil at 0-40 cm depth was predominantly sandy loam (62.0% sand and 27.0% silt at CARDI, and 58.8% sand and 29.6% silt at PNG) with the presence of clay (~20%) increasing in the 40-60 cm soil layer. At CARDI, soil pH in 2016 pre-planting was 6.72 and 7.12 at 0-20 cm and 20-50 cm depth, respectively. At PNG, soil pH in 2016 pre-land preparation was 5.36 at 0-20 cm depth and averaged 5.91 in the 20-60 cm soil layer. More details regarding the physico-chemical properties of the soils at both sites can be found in Table 2 in Ballester et al. [6]. One experiment was conducted per site in the 2016/17 dry season. In the 2017/18 dry season, one experiment was conducted at CARDI while two parallel experiments were conducted at PNG. One experiment was conducted per site in the 2016/17 dry season. In the 2017/18 dry season, one experiment was conducted at CARDI while two parallel experiments were conducted at PNG. Experiment 1 was conducted at PNG to investigate (i) the effect that fertilizer placement could have on crop nutrient availability caused by poor lateral water movement from furrows into the center of the beds, and (ii) the effect of different types of organic amendments on peanut yield. Fertilizer was placed in the middle of the beds (F1) and along the edge of the bed, slightly offset from the seeding row and below seeds (F2). The soil amendment treatments tested were: (C) control, no soil amendment, (SB) rice straw at 5 t ha −1 and (M) surface spread cow/goat manure at 20 t ha −1 . Manure was spread over the soil surface and incorporated into the soil during bed forming. Once beds were formed using a three-point linkage bed forming bar on a tractor (beds 0.30 m aside 0.25 m furrows), uncut rice straw was laid out in the depression formed in the center of each bed of the SB treatment and covered with soil recovered from the floor of the adjacent furrows. This created a buried subsurface residue layer at~0.10 m depth.
The experimental design was a three-by-two factorial randomized block design with three replicates. Figure 2 illustrates the distribution of the treatments and dimensions of the site and plots.
On 7 and 8 December 2016, seeds of the L23 variety of peanut were sown at~2.0 cm depth by hand along the edge of each bed in two rows at a spacing of 0.30 m × 0.25 m and fertilizer (15:15:15 NPK) at 156 kg ha −1 was banded at a depth of~3.0 cm, offset and below the seeding depth. The site was hand-watered daily from sowing until 9 January 2017 when furrow irrigation commenced. Irrigation water had an average pH of 7.9 and an electrical conductivity (EC) of 0.07 dS m −1 for the season.
Average daily air temperature (Ta) during the 2016/17 peanut growing season was 26.0 • C. Minimum and maximum Ta recorded were 21.9 • C and 30.0 • C. Unseasonal rainfall events occurred on 21-28 January (~326 mm), on 3-14 February (~340 mm) and on [16][17][18][19][20][21][22][23][24][25] March (~471 mm) with the total rainfall over the season being 1171 mm. Total ET o was 474 mm. In the early crop stages, the crop was irrigated twice a week with an average total irrigation depth of 14 mm per plot and event. As the season progressed, irrigation frequency was adjusted to three days per week to account for the increasing evaporative demand and plant water requirements. The average cumulative total of irrigation water applied to each plot was 278 mm.

Experiment 2
Experiment 2 was conducted at CARDI. The experiment was a four-by-two factorial randomized block design with three replicates (Figure 2). The main treatments applied were (C) control, no soil amendment, (SB) rice straw at 10 t ha −1 buried in beds as a part of bed forming, (SI) rice straw at 10 t ha −1 and (B + M) biochar mixed with cow manure at 10 t ha −1 . Two inorganic fertilizer rates applied at sowing were also tested: (F1) 90N, 60P 2 O 5 , 30K 2 O (Urea 47 kg ha −1 , diammonium phosphate (DAP) 130 kg ha −1 and potassium chloride (KCl) 50 kg ha −1 ), and (F2) 135N; 90P 2 O 5 ; 45K 2 O (Urea 70.5 kg ha −1 , DAP 195 kg ha −1 , KCl 75 kg ha −1 ). In the SI plots, rice straw was spread and incorporated into the soil with a rotary hoe before bed forming. In the SB and B + M treatments, rice straw and biochar plus manure, respectively, were banded as part of the bed forming process. Fertilizers were banded in the middle of the bed in the F1 and F2 treatments.
On 17 January 2017, maize (variety CM1) was sown with a plant and row spacing of 0.30 m and 0.65 m, respectively. Germination success was low due to untimely rainfall that disrupted beds. The control treatment had the greatest germination success (48.9%), followed by B + M (36.75%), SI (35.6%) and SB (31.4%) treatments. Locations where germination had not occurred were re-sown on 25 January 2017. The site was hand-watered until two weeks after emergence when the crop was furrow-irrigated. soil surface and incorporated into the soil during bed forming. Once beds were formed using a three-point linkage bed forming bar on a tractor (beds 0.30 m aside 0.25 m furrows), uncut rice straw was laid out in the depression formed in the center of each bed of the SB treatment and covered with soil recovered from the floor of the adjacent furrows. This created a buried subsurface residue layer at ~0.10 m depth.
The experimental design was a three-by-two factorial randomized block design with three replicates. Figure 2 illustrates the distribution of the treatments and dimensions of the site and plots.

Figure 2.
Experimental layout during the 2016/17 dry season of experiment 1 at PNG (top) and experiment 2 at CARDI (bottom). Location of the soil water tension sensors in each experiment is indicated with the symbol "x". C = control; SB = rice straw buried; M = manure; B + M = biochar plus manure; SI = rice straw incorporated. F1 and F2 in the experiment at PNG indicate fertilizer placed in the middle of the bed and along the edge of the bed, respectively. At CARDI, F2 plots were fertilized with 1.5 times the rate applied in F1 plots.
During the 2016/17 maize growing season at CARDI (from 17 January to 10 April 2017), daily average Ta ranged from 24.5 • C to 31.9 • C and relative humidity from 55.7% to 98.0%. Total ET o and rainfall for the growing season were 386.1 mm and 124 mm, respectively. Most of the rainfall (75 mm) was recorded in a rain event at the end of the growing season which delayed harvest until 10 April 2017. The average cumulative total of irrigation water applied to each plot was 177 mm.  Experiment 4 was a complete randomized block design combining three bed structures (conventional bed/furrow, flat bed and narrow bed) with two irrigation treatments (furrow irrigation and sprinkler irrigation) ( Figure 3). Table 1 describes the treatments applied in experiments 3 and 4. Beds in treatments CB-FI, CB-SI and NB-FI were formed using a bed making equipment that was adjusted to form narrower beds in the case of the NB-FI treatment. For the flat bed treatment (FB-SI), once the soil had been ploughed, a bund was constructed surrounding the bay to retain irrigation water. Experiment 4 was a complete randomized block design combining three bed structures (conventional bed/furrow, flat bed and narrow bed) with two irrigation treatments (furrow irrigation and sprinkler irrigation) ( Figure 3). Table 1 describes the treatments applied in experiments 3 and 4. Beds in treatments CB-FI, CB-SI and NB-FI were formed using a bed making equipment that was adjusted to form narrower beds in the case of the NB-FI treatment. For the flat bed treatment (FB-SI), once the soil had been ploughed, a bund was constructed surrounding the bay to retain irrigation water. Peanut (variety L23) were sown on 25 December 2017 in a similar manner to the previous season. Basal fertilizer was banded in the middle of the bed following the F1 strategy of experiment 1.
Over the 2017/18 peanut growing season (25 December 2017 to 5 April 2018), minimum and maximum Ta recorded were 21.0 • C and 31.7 • C, respectively. In contrast with the 2016/17 dry season, and as typically observed for the geographic region where the study was conducted, rainfall was scarce and only 21.6 mm were recorded over the growing season.
Plots from experiments 3 and 4 were hand watered daily for two weeks after which the farm method of irrigation were established on 10 January 2018. Averaged amount of water supplied in experiment 3 was 400 mm. In experiment 4, due to differences in the delivery rate between outlets in the furrow irrigation system and the hose used for the sprinkler irrigation, the total amount of water applied in sprinkler-irrigated plots was 75% of that applied to furrow-irrigated plots. On average, furrow-irrigated and sprinkler-irrigated plots received a total amount of irrigation water of 414.0 mm and 311.8 mm, respectively.

Experiment 5
Experiment 5 was conducted at CARDI, where three irrigation treatments (furrow irrigation, sprinkler irrigation and over-bed irrigation) were tested in combination with three soil amendment treatments: (C) no amendment, (SB) rice straw banded at 10 t ha −1 after bed forming and (B + M) biochar plus cow manure at 10 t ha −1 . The experimental layout was a split plot design where irrigation was the main plot factor arranged in a randomized complete block design with three replicates and soil organic amendment was the second factor distributed as subplots within the irrigation treatments ( Figure 3). In the over-bed irrigation treatment, water was applied through furrows, but plots were designed to allow water to reach an over-bed level to ensure water reached the center of the beds. To avoid waterlogging conditions in this treatment due to water ponding in the plots for an extended time period, plots were drained 30 min after each irrigation event. Each irrigation plot consisted of nine beds (three per soil amendment treatment). Maize was sown at a plant and row spacing of 0.25 m and 0.65 m.
Basal fertilizer was applied at sowing in the middle of the beds in all treatments. P and K crop requirements were applied as diammonium phosphate and KCl upfront while N was split in three equal applications of urea throughout the growing season (23 January, 19 February and 13 March 2018) to provide a total 184-90-45 NPK kg ha −1 . The Agronomy 2021, 11, 1929 8 of 24 site was hand-watered every one or two days until emergence and then irrigated with the corresponding irrigation method.
Average daily Ta for the maize growing season was 28.0 • C with a minimum daily temperature of 18.1 • C recorded on 7 February 2018 and a maximum daily temperature of 37.6 • C reached later in the season on 17 April 2018. Total ET o and rainfall values recorded during this period were 544 mm and 39 mm, respectively. Average total water applied to the furrow and sprinkler-irrigated treatments (not monitored in the over-bed irrigation) was 236 mm and 209 mm, respectively.

Soil Water Tension
Soil water tension was monitored in all the experiments with the exception of experiment 3 by means of one to three Watermark sensors (Model 200SS, Irrometer Company inc., California USA) installed in the middle of the central beds at 15 cm depth (Figures 2 and 3). Sensors were connected to either 900M Irrometer dataloggers (Irrometer Company inc., California, USA) or Wi-Field loggers (Goanna Telemetry, Goondiwindi, QL, Australia), which sent data hourly to a cloud-based data storage, processing and internet interface in real time (Brinkhoff et al., 2017).

Aboveground and Belowground Biomass Development
Ground canopy cover (GCC) was monitored across the growing season in experiments 1 (on 11 dates), 3 (on 20 dates) and 4 (on 17 dates) using the app Canopeo [15]. Measurements were taken at three randomly selected locations within each plot to determine the average value for each treatment.
Aboveground biomass was measured in all the experiments 3-4 times across the season using at least six plants per amendment treatment. In experiments 1, 2, 3 and 5, belowground biomass was also assessed. These measurements were taken from the vegetative stage to harvest in peanut and from flowering to harvest in maize. In experiment 1, part way through the excavation, the roots of each plant were photographed in situ as an indicator of root system structure and then once the rest of the root system had been excavated and cleaned of soil, the root system of the plant was carefully laid out with a reference scale and photographed again. At a later stage, using the photographs, the length of roots in each plant in the 5-15 cm deep soil layer were measured manually. For experiments 1, 2, 3 and 5, after cleaning, aboveground and belowground parts were separated, and fresh weight recorded. Each sample was oven dried at 70 • C for 48 h, reweighed to obtain root dry weight, shoot dry weight, shoot-to-root ratio and width of the root system. In experiment 3, the root system of each plant was sectioned into three layers (0-5 cm, 5-15 cm and >15 cm depth) and roots from the 5-15 cm soil layer individually measured for length. Aboveground and belowground measurements in experiment 5 were only conducted in the furrow-irrigated treatment.

Yield and Water Productivity
Peanut were harvested on 4 April in 2017 and on 30 March in 2018. Pods from each plot were harvested and fresh weight determined. Dry pod weight and dry grain weight were determined by oven-drying a 1 kg sub-sample at~70 • C for 48 h.
Harvest in the maize experiments occurred on 10 April in 2017 and on 19 April in 2018. Plant samples were taken within each plot from a sampling area of 8.45 m 2 (52 plants) and fresh cob weight and grain yield at 14% moisture determined.
Water productivity was calculated as the ratio between grain yield and total amount of irrigation water applied (kg m −3 ).

Statistical Analysis
One-way and two-way analyses of variance (ANOVA) were used to determine whether there was a statistically significant difference in crop development, yield and water productivity among treatments. Significant differences between treatments was tested using the least significant difference (LSD) post-hoc test with the level of significance set at p ≤ 0.05.

Experiment 1 (PNG 2016-17)
Average values of soil water tension for each amendment treatment over the growing season are depicted in Figure 4. Control and amendment treatments responded similarly to irrigation and environmental conditions. The soil remained relatively wet during the time when the crop was hand watered and for two weeks after the establishment of furrow irrigation, until around the time of first flower emergence (18 January 2017; 43 days after sown, DAS). From that time, soil dried rapidly with minimal response to irrigation modifications (three irrigation events per week) or rainfall events. During February, the SB treatment (rice straw buried) retained a higher level of moisture compared to the other treatments. The apparent lower values of soil water tension in the SB treatment than in the other treatments could be the result of the buried straw layer intercepting the upward flux of water from the deeper soil, reducing its loss by evaporation. Only for the period from 16 to 25 March 2017 when significant rainfall events occurred (471 mm) did soil water tension in all treatments return to values close to zero, indicative of a saturated soil. The lack of response of the sensors to irrigation highlights the severity of the soil physical constrains to lateral movement of water in these rice-growing soils reported in Ballester et al. [6].

Statistical Analysis
One-way and two-way analyses of variance (ANOVA) were used to determine whether there was a statistically significant difference in crop development, yield and water productivity among treatments. Significant differences between treatments was tested using the least significant difference (LSD) post-hoc test with the level of significance set at p ≤ 0.05.

Experiment 1 (PNG 2016-17)
Average values of soil water tension for each amendment treatment over the growing season are depicted in Figure 4. Control and amendment treatments responded similarly to irrigation and environmental conditions. The soil remained relatively wet during the time when the crop was hand watered and for two weeks after the establishment of furrow irrigation, until around the time of first flower emergence (18 January 2017; 43 days after sown, DAS). From that time, soil dried rapidly with minimal response to irrigation modifications (three irrigation events per week) or rainfall events. During February, the SB treatment (rice straw buried) retained a higher level of moisture compared to the other treatments. The apparent lower values of soil water tension in the SB treatment than in the other treatments could be the result of the buried straw layer intercepting the upward flux of water from the deeper soil, reducing its loss by evaporation. Only for the period from 16 to 25 March 2017 when significant rainfall events occurred (471 mm) did soil water tension in all treatments return to values close to zero, indicative of a saturated soil. The lack of response of the sensors to irrigation highlights the severity of the soil physical constrains to lateral movement of water in these rice-growing soils reported in Ballester et al. [6]. A significantly greater GCC was observed in the treatment amended with manure (M) than in the C and SB in the measurements from 9 January to 13 February 2017 and the last measurement date (Figure 5a). Aboveground biomass measurements also indicated that manure application promoted biomass production in comparison to the addition of rice straw or no addition of organic matter in the early, mid-season although differences among treatments were not apparent at harvest (Table 2). This result is not surprising as the Mekong alluvial sandy loam soils typically have negligible levels of organic matter and clay, and very low CEC [16]. This makes these soils dependent on fertilizers for most A significantly greater GCC was observed in the treatment amended with manure (M) than in the C and SB in the measurements from 9 January to 13 February 2017 and the last measurement date (Figure 5a). Aboveground biomass measurements also indicated that manure application promoted biomass production in comparison to the addition of rice straw or no addition of organic matter in the early, mid-season although differences among treatments were not apparent at harvest (Table 2). This result is not surprising as the Mekong alluvial sandy loam soils typically have negligible levels of organic matter and clay, and very low CEC [16]. This makes these soils dependent on fertilizers for most nutrients to drive production. The application of cow manure at 5 t ha −1 in the M treatment in addition to the synthetic fertilizer at sowing most likely provided the crop with nutrients such as P and S (less likely N due to the crop N-fixing capacity) otherwise scarce in these soils. At harvest, there was a significant interaction between organic amendment and fertilizer placement on peanut biomass, which indicated peanut aboveground biomass to be less responsive to organic amendment when starter fertilizer was added in close proximity to the sowing row (F2) ( Table 3). This is probably the result of more optimal placement of fertilizer to meet plant requirement. Fertilizer placement did not influence GCC (Figure 5b).
nutrients to drive production. The application of cow manure at 5 t ha −1 in the M treatment in addition to the synthetic fertilizer at sowing most likely provided the crop with nutrients such as P and S (less likely N due to the crop N-fixing capacity) otherwise scarce in these soils. At harvest, there was a significant interaction between organic amendment and fertilizer placement on peanut biomass, which indicated peanut aboveground biomass to be less responsive to organic amendment when starter fertilizer was added in close proximity to the sowing row (F2) ( Table 3). This is probably the result of more optimal placement of fertilizer to meet plant requirement. Fertilizer placement did not influence GCC (Figure 5b).  "ns" denotes not statistically significant differences while "*" indicates significant differences at p ≤ 0.05. Different letters within a column denote significant differences between treatments. C = Control; SB = straw buried; M (manure).
Plant sampling for the belowground assessment revealed that peanut root system was typically shallow (15-35 cm depth) with lateral roots radiating out up to 60 cm. Similar to the results presented in Table 2, dry weight of shoots and roots in the M treatment appeared to be greater than in C and SB at maturity (22 March 2017) (Figure 6a,b). This, however, was not confirmed by the statistical analysis that did not detect significant differences between amendment or fertilizer treatments at any of the three sampling dates. Different letters within a measurement date indicate statistically significant differences (p < 0.05) between treatments. "ns" denotes not statistically significant differences. The order of the letters from top to bottom correspond with the order in which treatments are presented in the legend of each graph. Table 2. Two-way ANOVA for the effects of soil amendments and fertilizer placement on aboveground biomass of peanut (t ha −1 ) in experiment 1. "ns" denotes not statistically significant differences while "*" indicates significant differences at p ≤ 0.05. Different letters within a column denote significant differences between treatments. C = Control; SB = straw buried; M (manure). Plant sampling for the belowground assessment revealed that peanut root system was typically shallow (15-35 cm depth) with lateral roots radiating out up to 60 cm. Similar to the results presented in Table 2, dry weight of shoots and roots in the M treatment appeared to be greater than in C and SB at maturity (22 March 2017) (Figure 6a,b). This, however, was not confirmed by the statistical analysis that did not detect significant differences between amendment or fertilizer treatments at any of the three sampling dates. The partitioning of shoot and root carbohydrate at each sampling date consistently maintained a ratio of ~8:1 for the three sampling periods indicating that none of the treatments altered the ratio of biomass partitioning in favor of roots (Figure 6c). Nevertheless, the length of subsurface (5-15 cm depth) lateral roots measured at the first and third sampling dates was statistically (p < 0.05) greater in the SB than in the C and M treatments (Figure 6d). Observations made at both sampling dates indicated that roots in the SB treatment appeared not to populate the buried straw layer as it was expected but instead, populated the interface between the straw layer and the soil layer either above or below the buried rice straw layer. Although no differences in biomass were observed between treatments at harvest, the C treatment produced significantly (p < 0.05) more pod and grain yield than SB (Table  3). No statistically significant differences were observed between the C and M treatments. The reduction in grain yield associated with the buried straw treatment (SB) could be due to the induced nutrient deficiency that could occur in soil due to the breakdown of the high C:N rice straw. Placement of the fertilizer in relation to the crop at sowing did not influence yield and thus it was not further studied in the subsequent dry growing season. The partitioning of shoot and root carbohydrate at each sampling date consistently maintained a ratio of~8:1 for the three sampling periods indicating that none of the treatments altered the ratio of biomass partitioning in favor of roots (Figure 6c). Nevertheless, the length of subsurface (5-15 cm depth) lateral roots measured at the first and third sampling dates was statistically (p < 0.05) greater in the SB than in the C and M treatments (Figure 6d). Observations made at both sampling dates indicated that roots in the SB treatment appeared not to populate the buried straw layer as it was expected but instead, populated the interface between the straw layer and the soil layer either above or below the buried rice straw layer.

Aboveground Biomass
Although no differences in biomass were observed between treatments at harvest, the C treatment produced significantly (p < 0.05) more pod and grain yield than SB (Table 3). No statistically significant differences were observed between the C and M treatments. The reduction in grain yield associated with the buried straw treatment (SB) could be due to the induced nutrient deficiency that could occur in soil due to the breakdown of the high C:N rice straw. Placement of the fertilizer in relation to the crop at sowing did not influence yield and thus it was not further studied in the subsequent dry growing season.

Experiment 2 (CARDI 2016/17)
Drier soil was monitored in beds than in furrows in all the treatments (Figure 7a,b). Comparison of the soil water tension in beds among treatments showed that SI and particularly the B + M treatment retained a higher level of soil moisture during most of the growing season than the other two treatments (Figure 7a). Soil water tension was generally >30 kPa during the first half of the season. In early March, the soil tension differential between the furrows and beds was minimized in the B + M treatment. This was in contrast to the treatments amended with rice straw (SI and SB), which were intended to promote lateral hydraulic conductivity. This result indicates that treatment B + M was more effective in allowing lateral water movement.

Experiment 2 (CARDI 2016/17)
Drier soil was monitored in beds than in furrows in all the treatments (Figure 7a,b). Comparison of the soil water tension in beds among treatments showed that SI and particularly the B + M treatment retained a higher level of soil moisture during most of the growing season than the other two treatments (Figure 7a). Soil water tension was generally > 30 kPa during the first half of the season. In early March, the soil tension differential between the furrows and beds was minimized in the B + M treatment. This was in contrast to the treatments amended with rice straw (SI and SB), which were intended to promote lateral hydraulic conductivity. This result indicates that treatment B + M was more effective in allowing lateral water movement.
Root biomass assessment showed that plants from the B + M treatment had the highest root dry mass at harvest (10 April), although no statistically significant differences were found with respect to the other treatments (Table 4). Across all the treatments and at each sampling date, maize roots were typically shallow, between 0.15 m and 0.30 m deep, and made up mainly of primary roots. However, some plants produced adventitious roots emanating from the stem. Aboveground biomass was only affected at the last measurement date when it was significantly lower in the two straw treatments (SB and SI) compared with the unamended treatment (Table 4). Root biomass assessment showed that plants from the B + M treatment had the highest root dry mass at harvest (10 April), although no statistically significant differences were found with respect to the other treatments (Table 4). Across all the treatments and at each sampling date, maize roots were typically shallow, between 0.15 m and 0.30 m deep, and made up mainly of primary roots. However, some plants produced adventitious roots emanating from the stem. Aboveground biomass was only affected at the last measurement date when it was significantly lower in the two straw treatments (SB and SI) compared with the unamended treatment (Table 4).
At harvest, cob fresh weight in the C and B + M treatments was significantly higher than that obtained in the SI treatment (Table 5). Cob fresh weight was also higher according to fertilizer rate. Treatments C and B + M had the highest (p < 0.05) grain yield. None of the organic amendment treatments had any influence on the ratio of grain yield/stem fresh weight. Greater fertilization at sowing (F2) significantly promoted grain yield in relation to the stem fresh weight. The highest aboveground biomass and grain yield were obtained in the C and B + M treatments compared to the treatments amended with rice straw (SB and SI). One explanation for this could be that treatments SB and SI required replanting, causing a delay in development which persisted between these plants and the plants in treatments C and B + M over the duration of the experiment. A second explanation could Agronomy 2021, 11,1929 13 of 24 be that amendment in the SB and SI treatments with 10 t ha −1 of high C:N rice straw may have immobilized plant available nitrogen.

Experiment 3 (PNG 2017-18)
In experiment 3 conducted on peanut during the 2017/18 dry growing season, GCC of treatments where animal manure had been applied (M and M+SB) was greater (p < 0.05) than in the control treatment during a large part of the season (Figure 8).
This would suggest that although 156 kg ha −1 of NPK fertilizer was applied in all the treatments at sowing, the incorporated manure provided additional nutrients to the crop that were not available in soil nor supplied in the basal fertilizer. Despite leaf canopy being significantly greater in treatments that received manure compared to the control, statistically significant differences in the aboveground biomass were not observed at any of the four stages of the crop monitored (Table 6).

Experiment 3 (PNG 2017-18)
In experiment 3 conducted on peanut during the 2017/18 dry growing season, GCC of treatments where animal manure had been applied (M and M+SB) was greater (p < 0.05) than in the control treatment during a large part of the season (Figure 8). This would suggest that although 156 kg ha -1 of NPK fertilizer was applied in all the treatments at sowing, the incorporated manure provided additional nutrients to the crop that were not available in soil nor supplied in the basal fertilizer. Despite leaf canopy being significantly greater in treatments that received manure compared to the control, statistically significant differences in the aboveground biomass were not observed at any of the four stages of the crop monitored (Table 6).  In contrast to experiment 1, no significant differences were observed between treatments in root length in the 0.05-0.15 m soil layer in the 2017/18 dry growing season. On average, root length was 230.9 ± 36.1 cm at flowering and 281.0 ± 24.3 cm at maturity. However, the shoot to root ratio was greater (p < 0.05) in the M and M+SB treatments than in the C treatment ( Figure 9).  In contrast to experiment 1, no significant differences were observed between treatments in root length in the 0.05-0.15 m soil layer in the 2017/18 dry growing season. On average, root length was 230.9 ± 36.1 cm at flowering and 281.0 ± 24.3 cm at maturity. However, the shoot to root ratio was greater (p < 0.05) in the M and M+SB treatments than in the C treatment (Figure 9).

Vegetative Flowering Pod Development Maturity
At harvest, neither pod fresh weight, grain fresh weight, nor grain dry weight of peanut were statistically affected by the organic amendments (Table 7). Water productivity was~35% lower in the treatments featuring incorporated manure (M and M + SB caused by luxuriant growth of leaf canopy (Figure 8) due to less biotic stress than the control plants. As a result, plants from the C treatment likely allocated more photosynthates to reproductive development than the M and M + SB treatments and matured earlier. Table 7. Average values of pod fresh weight (t ha −1 ), grain fresh weight (t ha −1 ), grain dry weight (t ha −1 ) and water productivity (kg mm −1 ) for each of the soil organic amendment treatments: (C) control, (M) manure at 20 t ha −1 and (M + SB) manure at 20 t ha −1 plus rice straw buried at 5 t ha −1 .  At harvest, neither pod fresh weight, grain fresh weight, nor grain dry weight of peanut were statistically affected by the organic amendments (Table 7). Water productivity was ~35% lower in the treatments featuring incorporated manure (M and M + SB caused by luxuriant growth of leaf canopy (Figure 8) due to less biotic stress than the control plants. As a result, plants from the C treatment likely allocated more photosynthates to reproductive development than the M and M + SB treatments and matured earlier. Table 7. Average values of pod fresh weight (t ha −1 ), grain fresh weight (t ha −1 ), grain dry weight (t ha −1 ) and water productivity (kg mm −1 ) for each of the soil organic amendment treatments: (C) control, (M) manure at 20 t ha −1 and (M + SB) manure at 20 t ha −1 plus rice straw buried at 5 t ha −1 .

Grain Fresh Weight
Grain Dry Weight Water Productivity  Figure 10 illustrates the average soil water tension for each combination of bed architecture and irrigation method tested in the 2017/18 dry growing season at PNG. Three apparent groups can be distinguished in this figure, with the sprinkler irrigation treatments (FB-SI and CB-SI) showing higher soil water tension values (drier soils) at 0.20 m depth for the entire season than the furrow-irrigated treatments. This higher average soil water tension was ascribed to less water being applied to the crop in the sprinkler-irrigated treatments than in the furrow-irrigated. tecture and irrigation method tested in the 2017/18 dry growing season at PNG. Three apparent groups can be distinguished in this figure, with the sprinkler irrigation treatments (FB-SI and CB-SI) showing higher soil water tension values (drier soils) at 0.20 m depth for the entire season than the furrow-irrigated treatments. This higher average soil water tension was ascribed to less water being applied to the crop in the sprinkler-irrigated treatments than in the furrow-irrigated. The furrow-irrigated treatments maintained wetter conditions throughout the growing season with the treatment with the narrow beds (NB-FI) having the lowest soil water tension values (Figure 10). This was mainly due to the differences in bed geometry between the CB-FI and NB-FI treatments. Having twice the number of furrows in the NB-FI treatment compared with the CB-FI as well as narrower beds meant that water could laterally transverse the bed from either side of the seeding row. Therefore, more water was available for the plants in the NB-FI than in the CB-FI treatment.

Experiment 4 (PNG 2017-18)
Measurements of the percentage of GCC showed that for most of the growing season, canopy development of peanut plants in the NB-FI treatment was significantly retarded in comparison to the other treatments ( Figure 11). This was more notable during the flowering early pegging period (mid-January to mid-February). However, the canopy of plants from the NB-FI treatment developed further as maturity approached, reaching similar values of GCC at that stage of the crop to those of the other treatments. The furrow-irrigated treatments maintained wetter conditions throughout the growing season with the treatment with the narrow beds (NB-FI) having the lowest soil water tension values (Figure 10). This was mainly due to the differences in bed geometry between the CB-FI and NB-FI treatments. Having twice the number of furrows in the NB-FI treatment compared with the CB-FI as well as narrower beds meant that water could laterally transverse the bed from either side of the seeding row. Therefore, more water was available for the plants in the NB-FI than in the CB-FI treatment.
Measurements of the percentage of GCC showed that for most of the growing season, canopy development of peanut plants in the NB-FI treatment was significantly retarded in comparison to the other treatments ( Figure 11). This was more notable during the flowering early pegging period (mid-January to mid-February). However, the canopy of plants from the NB-FI treatment developed further as maturity approached, reaching similar values of GCC at that stage of the crop to those of the other treatments.
Aboveground biomass did not significantly differ between treatments at any sampling date (Table 8). However, in the NB-FI treatment, it appeared delayed compared to the other treatments at the vegetative and flowering stages. This could be due to the sensitivity of pulse crops in general, and peanut in particular, to anoxic soil conditions associated with waterlogged soils [17]. Soil water tension in the NB-FI treatment where narrow beds were investigated remained close to or above field capacity (~30 kPa) for the first six weeks of the growing season (Figure 10), which may have detrimentally affected the early development of plants in this treatment.
Pod and grain weight appeared to be considerably higher in the FB-SI treatment (flat bed with sprinkler irrigation) than in the other treatments, although this result could not be statistically validated (Table 9). No statistically significant differences were detected either among treatments in water productivity. However, considerably higher water productivity was achieved in the two sprinkler-irrigated treatments (FB-SI and CB-SI) than in the furrow-irrigated plots (Table 9). Since~25% more water was applied in the furrow-irrigated treatments with no effect on yield, the higher apparent water productivity of the FB-SI and CB-SI treatments was most likely due to improved efficiencies as a product of less water losses associated with sprinkler irrigation. As drier soils were observed in the sprinkler-irrigated treatments than in the furrow-irrigated (Figure 10), it can be speculated that the higher level of osmotic stress imposed by the FB-SI and CB-SI treatments due to the lower availability of water might have led to greater amount of carbohydrate being channeled into reproductive development and grain production. Aboveground biomass did not significantly differ between treatments at any sampling date (Table 8). However, in the NB-FI treatment, it appeared delayed compared to the other treatments at the vegetative and flowering stages. This could be due to the sensitivity of pulse crops in general, and peanut in particular, to anoxic soil conditions associated with waterlogged soils [17]. Soil water tension in the NB-FI treatment where narrow beds were investigated remained close to or above field capacity (~30 kPa) for the first six weeks of the growing season ( Figure 10), which may have detrimentally affected the early development of plants in this treatment. Table 8. Average aboveground biomass measured at four stages of the crop in each combination of bed architecture and irrigation method tested in the 2017/18 dry growing season: (CB-FI) conventional bed/furrow system with furrow irrigation, (FB-SI) flat bed with sprinkler irrigation, (CB-SI) conventional bed/furrow with sprinkler irrigation and (NB-FI) narrow beds with furrow irrigation. Pod and grain weight appeared to be considerably higher in the FB-SI treatment (flat bed with sprinkler irrigation) than in the other treatments, although this result could not be statistically validated (Table 9). No statistically significant differences were detected either among treatments in water productivity. However, considerably higher water productivity was achieved in the two sprinkler-irrigated treatments (FB-SI and CB-SI) than in the furrow-irrigated plots (Table 9). Since ~25% more water was applied in the Figure 11. Average percentage of canopy ground cover (GCC) for the treatments assessed in experiment 4: conventional bed/furrow system with furrow irrigation (CB-FI), flat bed with sprinkler irrigation (FB-SI), conventional bed/furrow with sprinkler irrigation (CB-SI) and narrow beds with furrow irrigation (NB-FI). Different letters within a measurement date indicate statistically significant differences (p < 0.05) between treatments. The order of the letters from top to bottom correspond with the order in which treatments are presented in the legend. "ns" denotes not statistically significant differences.   Table 9. Average values of pod fresh weight (t ha −1 ), grain dry weight (t ha −1 ) and water productivity (kg mm −1 ) for each combination of bed architecture and irrigation method tested in the 2017/18 dry growing season: (I1) conventional bed/furrow system with furrow irrigation, (I2) flat bed with sprinkler irrigation, (I3) conventional bed/furrow with sprinkler irrigation and (I4) narrow beds with furrow irrigation.

Experiment 5 (CARDI 2017/18)
Despite all plots being watered regularly, drier soils were generally experienced by the over-bed and sprinkler-irrigated treatments rather than the furrow-irrigated plots ( Figure 12). The application of rice straw and biochar/manure amendments prior to sowing generally improved soil moisture retention. This effect was more marked in the treatment with rice straw banded and buried at 10 t ha −1 (SB) for all the replicates within the furrow-irrigated treatment, which had the lowest soil water tension values over the season. This result was consistent with the previous seasons findings at PNG. Although grain yield in the B + M treatment on average was 11% higher than in the SB treatment, and apparent grain yield appeared lower in the over-bed treatment compared to the sprinkler and furrow-irrigated treatments, there were no statistically significant differences in grain yield among amendment and irrigation treatments ( Table 10). Comparison of the water productivity between the sprinkler and furrow irrigation treatments, when the amount of water applied was monitored for each plot individually, showed that sprinkler-irrigated plots had significantly higher water productivity (Table  10). Table 10. Average grain yield (t ha −1 ) and water productivity of maize for the irrigation and amendment (control (C), buried rice straw (SB) and biochar plus manure (B + M)) treatments and each combination of irrigation and amendment tested in experiment 5 during the 2017/18 dry season.

Grain Dry Weight
Water Productivity Irrigation treatments ns * Furrow irrigation (FI) 2.07 8.76 Although grain yield in the B + M treatment on average was 11% higher than in the SB treatment, and apparent grain yield appeared lower in the over-bed treatment compared to the sprinkler and furrow-irrigated treatments, there were no statistically significant differences in grain yield among amendment and irrigation treatments (Table 10). Comparison of the water productivity between the sprinkler and furrow irrigation treatments, when the amount of water applied was monitored for each plot individually, showed that sprinkler-irrigated plots had significantly higher water productivity (Table 10). Table 10. Average grain yield (t ha −1 ) and water productivity of maize for the irrigation and amendment (control (C), buried rice straw (SB) and biochar plus manure (B + M)) treatments and each combination of irrigation and amendment tested in experiment 5 during the 2017/18 dry season.

Grain Dry Weight
Water Productivity Comparing the effect that irrigation treatments had on aboveground biomass, the overbed treatment had significantly (p < 0.05) lower aboveground biomass than the sprinkler and furrow-irrigated treatments on 5 March and 29 March 2018 ( Figure 13). On the later sampling date, maize plants from the treatment amended with a mix of biochar and manure had the highest aboveground biomass (88.3 g plant −1 ) with statistically significant (p < 0.05) differences recorded between this and the treatment amended with rice straw (SB; 71.6 g plant −1 ). Comparing the effect that irrigation treatments had on aboveground biomass, the over-bed treatment had significantly (p < 0.05) lower aboveground biomass than the sprinkler and furrow-irrigated treatments on 5 March and 29 March 2018 ( Figure 13). On the later sampling date, maize plants from the treatment amended with a mix of biochar and manure had the highest aboveground biomass (88.3 g plant −1 ) with statistically significant (p < 0.05) differences recorded between this and the treatment amended with rice straw (SB; 71.6 g plant −1 ). Assessment of root and shoot biomass within the furrow-irrigated treatment from flowering to harvest did not show any significant difference in root or shoot dry weight, shoot to root ratio, root depth nor roots system width as a function of soil organic amendments ( Figure 14). Assessment of root and shoot biomass within the furrow-irrigated treatment from flowering to harvest did not show any significant difference in root or shoot dry weight, shoot to root ratio, root depth nor roots system width as a function of soil organic amendments ( Figure 14).

General Discussion
Soil water tension recorded in this study in experiments 1 and 2 confirmed the constraint reported in Ballester et al. [6] of poor lateral movement of water in rice-growing soils typical of the lowlands of the lower Mekong basin. The lateral movement of water is of importance for crops grown on a "conventional" bed and furrow irrigation system as typically undertaken for dry season crops in both Laos and Cambodia. While strategies such as plant placement in furrows and side of beds could overcome the lack of access of roots to water, these approaches increase waterlogging risk. The current study showed that in bed and furrow systems, improvement of plant access to water can be relatively easily achieved by modifying bed architecture. Narrowing beds increased soil moisture availability for plants ( Figure 10) which would likely be of benefit for maize and other non-pulse crops. However, in the case of peanuts, this intervention resulted in the soil becoming too wet, particularly during the vegetative, flowering and early pegging stage, Figure 14. Biomass expressed in dry weight (g plant −1 ) of shoots (a), roots (b) and shoot-to-root ratio (c) as a function of organic amendments (none (C), manure (M) and manure plus rice straw buried (M + SB)) at three crop stages (flowering, cob formation and maturity) within the furrow-irrigated treatment in the 2017/18 dry season.

General Discussion
Soil water tension recorded in this study in experiments 1 and 2 confirmed the constraint reported in Ballester et al. [6] of poor lateral movement of water in rice-growing soils typical of the lowlands of the lower Mekong basin. The lateral movement of water is of importance for crops grown on a "conventional" bed and furrow irrigation system as typically undertaken for dry season crops in both Laos and Cambodia. While strategies such as plant placement in furrows and side of beds could overcome the lack of access of roots to water, these approaches increase waterlogging risk. The current study showed that in bed and furrow systems, improvement of plant access to water can be relatively easily achieved by modifying bed architecture. Narrowing beds increased soil moisture availability for plants ( Figure 10) which would likely be of benefit for maize and other non-pulse crops. However, in the case of peanuts, this intervention resulted in the soil becoming too wet, particularly during the vegetative, flowering and early pegging stage, which reduced both vegetative ( Figure 11) and reproductive development (Table 8). Delivering more frequent but lower volumes of irrigation per event as with sprinkler irrigation would likely be a preferred irrigation technique for peanuts. Further, this practice may potentially lead to saving water (25% savings were obtained compared with furrow irrigation in experiment 4) and boosting water productivity on lowland soils. The availability of nutrients supplied to plants as inorganic fertilizer at sowing could be also compromised by the poor lateral movement of water observed in these soils. However, results obtained in experiment 1 where fertilizer placement was assessed was inconclusive.
In a conventional bed and furrow irrigation system, it was hypothesized that the inclusion of a layer of straw buried below the topsoil would enhance the lateral movement of water into beds and increase soil moisture retention. However, in experiment 2 at CARDI, B + M treatments provided greater soil moisture retention and improved lateral water movement from furrows to the center of beds compared with rice straw. In the case of peanut, it was considered that including a layer of straw could enhance root development, allowing the plant to develop a larger root system and access more water. This effect has been commonly observed where the roots of the current crop exploit stable bio-pores remaining from previous crops [18]. Results in experiment 1 indicated that the presence of rice straw in the layer about 0.05 m beneath the bed surface promoted the length of lateral roots emanating from the main root at this depth band (Figure 6d). This could be due to a reduced penetration resistance in the top 0.20 m soil layer observed in the amended treatments in comparison to the control that prevented the soil from forming a thick cemented layer. Results from experiments 1 and 2 also showed that although a below ground layer of straw had in general a positive effect on soil moisture retention compared with a non-amended soil, the consequence of burying high C:N ratio rice residues is likely to cause tie up of N and P that may prevent the crop to have access to these nutrients. N fertilizer immobilization resulting from incorporation of residues with low N contents and high C:N ratio has been generally reported for rice-based cropping systems in the tropics [19]. Incorporating animal manure to the treatment with rice straw, which could negate any risk of nutrient tie up, was posed in this study as a practice that could overcome this possible issue. Similar strategies integrating the use of amendments, including chemical fertilizers and organic ameliorants, have been reported as beneficial for crops [20]. However, attempts to prove this in experiment 3 failed when root length in the affected zone was unaffected by any treatment and crop yield by peanut growing in soil amended with animal manure was less than that of plants growing in unamended soil. Clay-based soil amendments with manure have been considered by other authors to improve nutrient availability, soil water retention and productivity of crops [12,21,22]. The cost and low availability of clay-based amendments in Cambodia and Laos, however, makes this option less likely to be adopted by smallholders. Simulations of grain production by maize grown in the rice-growing lowlands have shown yields to range from 2.13−1.99 t ha −1 with an average grain yield of 2.11 t ha −1 [23]. However, in this study, several treatments examined in experiment 5 produced crops with grain yields well above the average simulated yield for these soils. Treatments leading to actual crop yields exceeding model predictions included those featuring biochar and manure under traditional furrow irrigation (2.39 t ha −1 ) and rice straw combined with sprinkler irrigation (2.34 t ha −1 ). These findings indicated that other crop management interventions exist to enhance maize production on lowland soils across Cambodia and Laos and present an opportunity by which smallholder maize yields may be increased. It seems likely that narrow beds and the addition of stable organic amendments such as rice hull biochar may provide yield enhancement through improved water dynamics as well as enhanced retention of mobile nutrients. Heavy applications of animal manures may contribute to maize production through the increased availability of plant essential nutrients. Further research is needed to verify the mechanism and extent by which amendments of readily available organic sources can augment further maize yields on the extensive areas of these soil types across Cambodia and Laos.
Contrary to the findings in maize, simulations using AquaCrop showed average peanut yields across Champassak province to be 3.76 t ha −1 , and for the three provinces in southern Cambodia, 2.69 t ha −1 [23]. The maximum grain yield attained in peanut in this study (Champassak province) was 1.87 t ha −1 . This indicates that the strategies tested here were only producing peanut crops capable of achieving yields 50% of potential. Previous research on peanut production [6], established crop water requirements and irrigation frequency for peanut crops when growing on these soils. Shorter irrigation intervals had positive effects on yields, largely due to the poor lateral water movement indicated above with more frequent applications of less water tending to "pulse" applied water into the root zone. The gap between actual and potential yields obtained with AquaCrop indicates factors other than water to be restraining actual crop yields. While basal fertilizer application at sowing met crop needs for N, P and K, it is likely that other essential nutrients may have been lacking. It was assumed that heavy applications of animal manures may help crops overcome deficiencies in other essential nutrients. However, the inability of animal manures to make up for other nutrient deficiencies indicates either a lack of appropriate nutrients in this material, or a lack of adequate soil microbial activity able to mineralize and release the required nutrients in a plant available form at a rate required by peanuts.

Conclusions
In this study, the use of organic interventions, bed architecture and irrigation methods in rice-growing lowland soils to overcome the poor lateral movement of water into beds observed in dry-season crops grown in a bed/furrow system was assessed in peanut and maize crops.
Narrowing beds increased soil moisture availability for plants. Although this strategy was shown not to be appropriate for peanut, it could be of interest in non-pulse crops that could have a market space in Cambodia and Laos. For peanut production, sprinkler irrigation would be recommendable to prevent the soil to remain near saturation for long periods and to improve water productivity.
Incorporation of rice straw into beds could be other strategy to be considered to enhance soil moisture retention and root development. This strategy, however, may prevent the crop from having access to nutrients, and its use should be accompanied by a source of nutrients that could negate any risk of nutrient tie up. In this study, however, incorporation of manure along with the rice straw did not have a positive effect on root development and crop performance.
The study showed that the addition of organic amendments such as biochar and manure may enhance maize production on lowland soils above the average simulated yield for these soils. These findings present opportunities to enhance maize production on lowland soils across Cambodia and Laos. The contrary, however, was observed for peanut, which indicates that factors other than water detrimentally affect crop yields. This could be related to a lack of essential nutrients other than N, P and K. Further research is needed to find management strategies that could bridge the identified gap between potential and actual peanut yields.