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Soil management practice effect on water balance of a dryland soil during fallow period on the Loess Plateau of China

机译:黄土高原休耕期土壤管理实践对水分平衡的影响

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To understand the mechanisms affecting water balance partitioning during fallow on drylands could improve the fallow management practices in arable land ecosystems. A three-year field experiment was conducted to evaluate the effects of field management regimes on water balance partitioning and fallow efficiency during the fallow periods under a winter wheat (Triticum aestivum L.) fallow system on the Loess Plateau, China. The fallow management regimes tested were: (i) conventional practice, (ii) catch cropping, and (iii) no tillage with wheat straw mulching. A process-oriented ecosystem model (CoupModel) was calibrated with field measurements and then used to generate comparative simulations of the water balance partitioning. The simulations indicated that mulching increased the soil water storage change by 38–71 mm during the three fallow periods, thus resulting in higher fallow efficiency by 9–12%, and decreased soil evaporation by 22–72 mm, compared with the conventional practice. Furthermore, water reached deeper horizons, resulting in 7 mm deep percolation in a wet year under mulching but not under conventional practice or catch cropping. The simulation results also showed that the catch cropping decreased the soil water storage change by 13–21 mm , although it lowered soil evaporation by 11–51 mm, and altogether reduced the fallow efficiency by 3–9%, compared to conventional practice. On the Loess Plateau of China mulching proved to be a sound measure for ensuring certain fallow efficiency and possibly benefit to the water cycle, while catch cropping negatively partitioned the water balance. The catch cropping under mulching might be another management regime to be considered.
机译:了解影响旱地休耕期间水平衡分配的机制可以改善耕地生态系统中的休耕管理实践。在中国黄土高原的冬小麦休耕制度下,进行了为期三年的田间试验,以评估田间管理制度对休耕期水分平衡分配和休耕效率的影响。所测试的休耕管理制度为:(i)常规做法,(ii)种植作物,以及(iii)不用麦秸覆盖耕作。通过现场测量对面向过程的生态系统模型(CoupModel)进行了校准,然后将其用于生成水平衡分配的比较模拟。模拟结果表明,与常规做法相比,覆盖在三个休耕期将土壤储水量变化增加了38–71 mm,从而使休耕效率提高了9–12%,土壤蒸发减少了22–72 mm。此外,水到达更深的地平线,在覆盖的情况下,在潮湿的一年中会产生7毫米的深层渗漏,但在常规做法或捕获作物下则不会。模拟结果还表明,与常规做法相比,捕捞作物可将土壤水储量变化减少13–21 mm,尽管可将土壤蒸发量减少11–51 mm,并将休闲效率降低3–9%。在中国的黄土高原,覆盖被证明是确保一定的休耕效率并可能有益于水循环的有效措施,而农作物对水的平衡分配不利。覆盖下的农作物种植可能是要考虑的另一种管理制度。

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