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在 projected climate change scenarios 下,基于微流域的综合农业系统中的径流量和土壤侵蚀,以及东喜马拉雅山生态系统(印度)的适应策略。

Runoff and soil erosion in the integrated farming systems based on micro-watersheds under projected climate change scenarios and adaptation strategies in the eastern Himalayan mountain ecosystem (India).

机构信息

Division of System Research and Engineering, ICAR Research Complex for NEH Region, Umiam, Meghalaya, 793 103, India.

Division of System Research and Engineering, ICAR Research Complex for NEH Region, Umiam, Meghalaya, 793 103, India.

出版信息

J Environ Manage. 2022 May 1;309:114667. doi: 10.1016/j.jenvman.2022.114667. Epub 2022 Feb 12.

Abstract

Land degradation caused by soil erosion (SE) in forests converted into cropland under climate change, particularly with increased rainfall intensity, is of great concern to the agricultural sustainability of the tropical mountain ecosystem. We evaluated the response of six hilly micro-watersheds (HMW) under different Integrated Farming Systems (IFSs) to SE in multi-model climate change scenarios using the Water Erosion Prediction Project (WEPP) model. The IFSs were forestry (HMW), abandoned shifting cultivation (HMW), livestock with fodder crops (HMW), agroforestry (HMW), agri-horti-silvi-pastoral (HMW), and horticulture (HMW) established on a hilly slope (32.0-53.2%) of the eastern Himalayas (Meghalaya, India). The WEPP model was calibrated and validated with measured runoff and soil loss data of 24 years for each of the six IFSs. The projected annual SE (average) for all HMWs increased in all RCPs. The IFS based on shifting cultivation (HMW) was the most vulnerable, with the highest percentage increase in SE (46-235%) compared to the baseline years (1976-2005) under RCP 8.5. The cultivated IFSs (HMW to HMW) had 47.8-57.0% less runoff and 39.2-74.6% less soil loss than HMW under RCP 8.5. Of these, HMW followed by HMW and HMW were the most effective at minimizing soil loss. Simulation results showed a reduction in soil loss through adaptive strategies such as mulching with broom grasses, stones, field beans, and the introduction of subsurface drainage. Adoption of IFS based on horticulture and agroforestry with bio-mulching on steep slopes is an effective measure to control soil erosion in the eastern Himalaya (India).

摘要

在气候变化下,森林转化为农田导致的土壤侵蚀(SE),尤其是降雨强度增加,对热带山地生态系统的农业可持续性构成了极大的威胁。我们使用水蚀预测项目(WEPP)模型,评估了六种不同的综合农业系统(IFS)下的丘陵小流域(HMW)对多模式气候变化情景下土壤侵蚀的响应。IFS 包括林业(HMW)、废弃轮作(HMW)、饲料作物养殖(HMW)、农林复合(HMW)、农林牧复合(HMW)和园艺(HMW),这些都建立在印度东北部喜马拉雅山脉(梅加拉亚邦)丘陵坡地(32.0-53.2%)上。我们用 WEPP 模型对这六种 IFS 进行了校准和验证,每个模型都有 24 年的径流量和土壤流失测量数据。在所有 RCP 中,所有 HMW 的预测年平均土壤侵蚀都有所增加。基于轮作的 IFS(HMW)最为脆弱,与基线年(1976-2005 年)相比,在 RCP 8.5 下,土壤侵蚀增加了 46-235%。在 RCP 8.5 下,与 HMW 相比,耕作 IFS(HMW 到 HMW)的径流量减少了 47.8-57.0%,土壤流失减少了 39.2-74.6%。其中,HMW、HMW 和 HMW 对减少土壤流失最为有效。模拟结果表明,通过采用覆盖作物扫帚草、石头、田豆和地下排水等适应性策略,可以减少土壤流失。在陡坡上采用基于园艺和农林复合的 IFS 并进行生物覆盖是控制印度东北部喜马拉雅山土壤侵蚀的有效措施。

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