首页> 外文期刊>Journal of Hydrology >Trajectory based detection of forest-change impacts on surface soil moisture at a basin scale [Poyang Lake Basin, China]
【24h】

Trajectory based detection of forest-change impacts on surface soil moisture at a basin scale [Poyang Lake Basin, China]

机译:基于轨迹的流域尺度森林变化对表层土壤水分影响的检测[[阳湖盆地,中国]

获取原文
获取原文并翻译 | 示例
           

摘要

Surface soil moisture plays a critical role in hydrological processes, but varies with both natural and anthropogenic influences. Land cover change unavoidably alters surface property and subsequent soil moisture, and its contribution is yet hard to isolate from the mixed influences. In combination with trajectory analysis, this paper proposes a novel approach for detection of forest-change impacts on surface soil moisture variation with an examination over the Poyang Lake Basin, China from 2003 to 2009. Soil moisture in permanent forest trajectory represents a synthetic result of natural influences and serves as a reference for isolating soil moisture alternation due to land cover change at a basin scale. Our results showed that soil moisture decreased in all forest trajectories, while the absolute decrease was lower for permanent forest trajectory (2.53%) than the whole basin (2.61%), afforestation trajectories (2.70%) and deforestation trajectories (2.81%). Moreover, afforestation has a high capacity to hold more soil moisture, but may take more than 6 years to reach its maximum capacity. Soil moisture increased from 14.09% to 14.94% for the afforestation trajectories with tree aging from 1 to 6 years. Finally, land cover change may affect soil moisture alternation toward different transformation directions. Absolute soil moisture decreases by 0.08% for the whole basin, 0.17% for afforestation and 0.28% for deforestation trajectories, accounting for 3.13%, 6.47% and 10.07% of the total decrease in soil moisture. More specifically, the transformation from woody Savannas, cropland and other lands to forest generated absolute soil moisture deceases of 0.20%, -0.08% and 0.27%, accounting for 7.26%, -3.52% and 9.57% of the decreases. On the other hand, the reverse transformation generated soil moisture deceases of 0.29%, 0.21% and 0.35%, accounting for 10.43%, 7.69% and 12.14% of the total decrease. Our findings should be valuable for evaluating the impacts of land cover change on soil moisture alternation and promoting effective management of water resources.
机译:表层土壤水分在水文过程中起着至关重要的作用,但会随自然和人为因素而变化。土地覆盖的变化不可避免地会改变表面特性和随后的土壤湿度,但其贡献仍难以与混合影响区分开。结合轨迹分析,本文提出了一种新的方法来检测森林变化对地表土壤水分变化的影响,方法是对2003年至2009年的2009阳湖流域进行考察。永久性森林轨迹中的土壤水分代表了综合的结果。自然影响,并为隔离流域尺度上土地覆盖变化引起的土壤水分变化提供参考。我们的结果表明,土壤水分在所有森林轨迹中都下降了,而永久性森林轨迹(2.53%)的绝对下降低于整个盆地(2.61%),造林轨迹(2.70%)和森林砍伐轨迹(2.81%)。此外,绿化具有保持更多土壤水分的高能力,但可能需要6年以上的时间才能达到最大能力。植树造林从1年到6年,土壤湿度从14.09%增加到14.94%。最后,土地覆盖变化可能会影响土壤水分向不同转化方向的交替。整个流域的绝对土壤水分减少了0.08%,造林的减少了0.17%,毁林轨迹的减少了0.28%,分别占土壤总减少量的3.13%,6.47%和10.07%。更具体地说,从木质的稀树草原,农田和其他土地向森林的转变产生的绝对土壤水分减少量为0.20%,-0.08%和0.27%,分别占减少量的7.26%,-3.52%和9.57%。另一方面,反向转化使土壤水分减少了0.29%,0.21%和0.35%,分别占总减少量的10.43%,7.69%和12.14%。我们的发现对于评估土地覆被变化对土壤水分交替的影响以及促进水资源的有效管理具有重要的价值。

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