Predicting integrated effects of subsurface drainage and climate change on water balance and nitrate losses

IF 5.7 3区 环境科学与生态学 Q1 WATER RESOURCES
Samira Ziaeifar, Ali Shahidi, Amir-Ashkan Malakshahi, Abdullah Darzi-Naftchali, Mehdi Nadi
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Abstract

To ensure the continued contribution of agriculture to global food security, food production systems must adapt to the challenges posed by environmental degradation and climate change. This study assesses the potential impacts of climate change on drainage systems, water balance, and nitrate loss in the consolidated paddy fields of a humid region. Using climate projections downscaled from earth system models (NorESM2 and CanESM5) under two shared socioeconomic pathways (SSP126 and SSP585), we analyzed expected changes in temperature, precipitation, and evapotranspiration (ET) over three canola growing seasons. The DRAINMOD model, calibrated for local conditions, was used to simulate water balance and nitrate losses for two subsurface drainage systems with a drain depth (D) of 0.65 m and spacings (L) of 15 m and 30 m (D0.65L15 and D0.65L30). Results showed a projected increase in minimum and maximum temperatures by 0.66 °C and 1.0 °C, respectively, under SSP126, and by 0.74 °C and 1.5 °C under SSP585, compared to the baseline period. ET is expected to increase by 7.3% under SSP126 and 8.1% under SSP585, resulting in total ET of 312.6 mm and 334.3 mm, respectively, compared to 306.4 mm in the base period. Precipitation during the growing season is projected to increase by 181.3 mm under SSP126, but decrease by 15.7 mm under SSP585, leading to shifts in drainage intensity. Nitrate losses under the climate change scenarios are expected to decrease slightly, with total losses in the D0.65L15 system dropping from 9.13 kg ha−1 in the baseline period to 7.15 kg ha−1 under SSP585. These findings highlight the need for optimizing drainage design to manage increased ET and varying precipitation patterns, ensuring environmental sustainability in the face of climate change.

预测地下排水和气候变化对水平衡和硝酸盐损失的综合影响
为确保农业继续为全球粮食安全作出贡献,粮食生产系统必须适应环境退化和气候变化带来的挑战。本研究评估了气候变化对湿润地区固结稻田排水系统、水分平衡和硝酸盐流失的潜在影响。利用地球系统模型(NorESM2和CanESM5)在两个共享的社会经济路径(SSP126和SSP585)下的气候预估,我们分析了三个油菜生长季节的温度、降水和蒸散(ET)的预期变化。根据当地条件进行校准的DRAINMOD模型,用于模拟两个地下排水系统的水平衡和硝酸盐损失,排水深度(D)为0.65 m,间距(L)为15 m和30 m (D0.65L15和D0.65L30)。结果显示,与基线期相比,SSP126和SSP585预计的最低和最高气温分别增加0.66°C和1.0°C, 0.74°C和1.5°C。预计在SSP126和SSP585下,ET分别增加7.3%和8.1%,导致总ET分别为312.6 mm和334.3 mm,而基期为306.4 mm。SSP126模式下生长季降水增加181.3 mm, SSP585模式下降水减少15.7 mm,导致降水强度发生变化。气候变化情景下的硝酸盐损失预计将略有减少,D0.65L15系统的总损失将从基线期的9.13 kg ha - 1降至SSP585情景下的7.15 kg ha - 1。这些发现强调了优化排水设计的必要性,以管理增加的ET和变化的降水模式,确保面对气候变化的环境可持续性。
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来源期刊
Applied Water Science
Applied Water Science WATER RESOURCES-
CiteScore
9.90
自引率
3.60%
发文量
268
审稿时长
13 weeks
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