Observations and management implications of crop and water interactions in cold water-limited regions

IF 5.9 1区 地球科学 Q1 ENGINEERING, CIVIL
Phillip Harder, Warren D. Helgason, Bruce Johnson, John W. Pomeroy
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Abstract

Crop and water interactions strongly influence crop production in water-limited dryland agricultural systems in cold regions, such as the Canadian Prairies. A water balance approach was used to quantify crop water use, identify the source of water and corresponding hydrological processes, and evaluate the effectiveness of management techniques to increase agricultural productivity. Detailed water balance observations for 19 site-years were collected at four sites. Crop water use was consistently greater than or equal to growing season precipitation and displayed substantial interannual variation. On average, growing season precipitation provided 66% of crop water use whilst antecedent soil moisture from water surpluses in shoulder and winter seasons and preceding wet years supplied the remainder. Up to 70% of crop water use was derived from non-growing season water sources when high precipitation winters preceded dry growing seasons. Observations of soil moisture, snow accumulation, precipitation, and evaporative fluxes showed substantial spatial and temporal variability in antecedent soil moisture contributions to crop growth, which has implications for agricultural management. The relative importance of antecedent soil water to crop growth decreased with increased growing season precipitation. The water balance observations were used to constrain the water-limited yield potential associated with the optimisation of stubble and crop residue management practices. Increasing retention of snowfall with stubble management and suppression of soil evaporation with increased crop residue cover was estimated to increase potential crop water availability on average by 20% but, depended on seasonal dynamics, ranging between 4 and 48%. These results articulate the complex interactions between cold and warm season hydrological processes that drive dryland agricultural production in Western Canada and constrain the potential for stubble and residue management practices to mitigate crop water extremes.
冷水受限地区作物与水相互作用的观测结果和管理影响
在加拿大大草原等寒冷地区,作物与水的相互作用对水资源有限的旱地农业系统中的作物产量影响很大。采用水平衡方法量化作物用水量,确定水源和相应的水文过程,并评估管理技术对提高农业生产率的有效性。在四个地点收集了 19 个地点年的详细水平衡观测数据。作物用水量始终大于或等于生长季降水量,且年际变化很大。平均而言,生长季降水量占作物用水量的 66%,其余部分由肩季、冬 季和之前潮湿年份的水分盈余所产生的先期土壤水分提供。在干旱生长季之前的高降水冬季,高达 70% 的作物用水来自非生长季水源。对土壤水分、积雪、降水量和蒸发通量的观测表明,前土壤水分对作物生长的贡献在空间和时间上存在很大差异,这对农业管理有一定影响。前土壤水分对作物生长的相对重要性随着生长季降水量的增加而降低。水量平衡观测结果被用于限制与优化茬口和作物残留物管理措施相关的水分限制产量潜力。据估计,通过留茬管理增加降雪滞留和通过增加作物秸秆覆盖抑制土壤蒸发可使作物潜在水分供应量平均增加 20%,但取决于季节动态,增加幅度在 4% 到 48% 之间。这些结果阐明了冷季和暖季水文过程之间复杂的相互作用,这种相互作用推动了加拿大西部的旱地农业生产,并限制了茬口和秸秆管理方法缓解作物极端需水量的潜力。
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来源期刊
Journal of Hydrology
Journal of Hydrology 地学-地球科学综合
CiteScore
11.00
自引率
12.50%
发文量
1309
审稿时长
7.5 months
期刊介绍: The Journal of Hydrology publishes original research papers and comprehensive reviews in all the subfields of the hydrological sciences including water based management and policy issues that impact on economics and society. These comprise, but are not limited to the physical, chemical, biogeochemical, stochastic and systems aspects of surface and groundwater hydrology, hydrometeorology and hydrogeology. Relevant topics incorporating the insights and methodologies of disciplines such as climatology, water resource systems, hydraulics, agrohydrology, geomorphology, soil science, instrumentation and remote sensing, civil and environmental engineering are included. Social science perspectives on hydrological problems such as resource and ecological economics, environmental sociology, psychology and behavioural science, management and policy analysis are also invited. Multi-and interdisciplinary analyses of hydrological problems are within scope. The science published in the Journal of Hydrology is relevant to catchment scales rather than exclusively to a local scale or site.
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