首页> 外文期刊>Field Crops Research >Simulated long-term effects of different soil management regimes on the water balance in the Loess Plateau, China.
【24h】

Simulated long-term effects of different soil management regimes on the water balance in the Loess Plateau, China.

机译:黄土高原地区不同土壤管理制度对水平衡的长期影响模拟。

获取原文
获取原文并翻译 | 示例
           

摘要

A soil management regime that improves water use efficiency (WUE) is urgently required to increase the sustainability of the winter wheat-summer fallow system in the Loess Plateau, China. However, the long-term partitioning of the water balance must be understood in order to evaluate the viability of possible soil management regimes. Therefore, an ecosystem model (CoupModel) was used to explore the effects on components of the water balance of five types of soil management regimes: conventional practice, wheat straw mulching, incorporation of high organic matter contents, compaction, and use of a harvested fallow crop. Three variants of the fallow crop approach were also considered, in which the crop was harvested 15, 30 and 45 days before sowing the wheat (designated Fallow-15 d, Fallow-30 d and Fallow-45 d, respectively). Simulations were used to identify the relative magnitude of soil evaporation, wheat transpiration and deep percolation and to elucidate the temporal variability in these components for a selected location using climate records spanning 45 years. However, the soil management regime significantly influenced the magnitude of every component of the water balance (in terms of minimum, maximum and mean values) over the long periods considered. Consequently, wheat yield and WUE differed significantly among the simulated treatments. Mulching led to significantly lower soil evaporation, higher transpiration, and more frequent and extensive deep percolation than other regimes, thereby improving fallow efficiency (percentage of rainfall stored in the soil during the fallow period at the end of the fallow period), wheat yields and WUE. In contrast, soil compaction gave the opposite results, leading to the most unfavourable partitioning of the water balance reflected in the lowest wheat yield and WUE values of all the regimes. In 90% of the years no deep percolation occurred in the soil compaction simulations. Use of a fallow crop with optimal harvest timing (Fallow-30 d) improved partitioning of the water balance (decreased soil evaporation) and did not significantly reduce wheat yield compared with conventional practice. High organic matter contents in the soil also had a positive influence on the water balance and improved wheat yield and WUE relative to conventional practice. Therefore, mulching appears to be the best management practice for the winter wheat-summer fallow system in the Loess Plateau, according to the simulations. Increasing soil organic matter may be the best option if mulching cannot be implemented. The ideal time for harvesting a fallow crop for use as green manure or fodder appears to be ca. 30 days before sowing the winter wheat..
机译:迫切需要一种提高水分利用效率(WUE)的土壤管理制度,以提高中国黄土高原冬小麦-夏季休耕系统的可持续性。但是,必须了解水平衡的长期分配,以便评估可能的土壤管理制度的可行性。因此,使用生态系统模型(CoupModel)探索五种土壤管理制度对水平衡成分的影响:常规做法,麦草覆盖,高有机质含量的掺入,压实和利用收获的休耕地作物。还考虑了休闲作物方法的三种变体,其中在播种小麦之前15、30和45天收获农作物(分别指定为Fallow-15 d,Fallow-30 d和Fallow-45 d)。通过使用模拟来确定土壤蒸发,小麦蒸腾作用和深层渗滤的相对量,并使用长达45年的气候记录来阐明选定地点这些成分的时间变异性。然而,在所考虑的长期内,土壤管理制度极大地影响了水平衡各组成部分的大小(就最小值,最大值和平均值而言)。因此,模拟处理之间的小麦产量和水分利用效率差异显着。覆盖比其他方式显着降低了土壤蒸发,蒸腾作用以及更频繁和广泛的深层渗滤,从而提高了休耕效率(休耕期结束时休耕期土壤中存储的降雨百分比),小麦产量和哇相反,土壤压实产生相反的结果,导致水分平衡的最不利分配反映在所有制度中最低的小麦产量和WUE值上。在90%的年份中,土壤压实模拟中未发生深层渗滤。与常规做法相比,使用具有最佳收获时机(Fallow-30 d)的休耕作物可以改善水平衡的分配(减少土壤蒸发),并且不会显着降低小麦产量。与常规做法相比,土壤中高有机质含量也对水平衡具有积极影响,并改善了小麦产量和水分利用效率。因此,根据模拟,覆盖似乎是黄土高原冬小麦-夏季休耕系统的最佳管理方法。如果不能覆盖地膜,增加土壤有机质可能是最好的选择。收获休闲作物用作绿肥或草料的理想时间大约为。播种冬小麦前30天

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号