松树林控制喜马拉雅地区土壤侵蚀的潜力--利用落尘放射性核素(137Cs)测量进行的研究

Anu David Raj , Suresh Kumar , Sankar Mariappan , K.R. Sooryamol , Justin George Kalambukattu
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摘要

喜马拉雅山拥有独特的地形,这要归功于数百万年来构造活动、地质侵蚀和沉积、冰川过程和气候影响的动态相互作用。崎岖陡峭的地形和不良的土地管理使其更容易受到水的侵蚀,对土壤造成负面影响,影响土壤生态系统所提供的产品和服务。在处理地形复杂的山坡时,用于土壤侵蚀评估的传统方法面临着局限性。使用放射性核素(FRN)-137Cs 为测量此类地形地区的土壤侵蚀情况提供了一种可行的替代方法。然而,喜马拉雅山西北部缺乏基于 137Cs 的土壤侵蚀研究。松树(Pinus roxburghii)是喜马拉雅山脉的主要森林类型,为自然生态系统和人类带来了诸多益处。在这项研究中,我们选择了喜马拉雅山地区松林覆盖的典型陡峭山坡进行土壤侵蚀评估。研究测得该地貌的 137Cs 参考库存量为 1409 Bq m-2。重要的是,沿山坡位置的 137Cs 浓度因地形变化而出现显著差异。坡形和坡度等地形因素被认为是丘陵山区土壤侵蚀的主要影响因素。山坡净土壤侵蚀率显示,山坡上部的净土壤侵蚀率最高,其次是山脊、山坡中部和山谷。松林下的净土壤侵蚀率介于 8.0 至 14.6 吨/公顷/年之间,平均为 9.9 吨/公顷/年。除上部山坡外,其他山坡位置的土壤侵蚀率均符合土壤流失容限(SLTL),表明上部山坡是需要采取适当保护措施的关键坡位。这项研究表明了森林在减轻土壤侵蚀、进而保护土壤资源方面的作用。研究结果为土地管理者和决策者提供了重要的见解和指导,强调了保护和恢复喜马拉雅山森林的必要性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Potential of pine forest in controlling soil erosion in Himalayan region - Investigation using fallout radionuclide (137Cs) measurements

Potential of pine forest in controlling soil erosion in Himalayan region - Investigation using fallout radionuclide (137Cs) measurements

The Himalayas possess a distinctive topography owe to the dynamic interplay of tectonic activity, geological erosion and sedimentation, glacial processes, and climatic influences over the millions of years. The rugged, steep terrain and poor land management make it more prone to water erosion, negatively impacts the soil, affecting the goods and services supported by the soil ecosystems. Traditional methods used in soil erosion assessment face limitations when dealing with topographically complex hillslopes. The use of Fallout Radionuclide (FRN) -137Cs provides a feasible alternative for measurement of soil erosion in the region with such topography. However, there is lack of 137Cs-based soil erosion studies in the north-west Himalayas. Pine (Pinus roxburghii) is the predominant forest type in the Himalayas, offering numerous benefits to both natural ecosystems and human beings. In this study, we selected a typical steep hillslope covered with pine forest in the Himalayas for soil erosion assessment. The study measured 137Cs reference inventory of 1409 Bq m−2 in the landscape. Importantly, the concentration of 137Cs along the hillslope positions showed a significant variation attributed to topographic variability. Topographic factors, such as the slope shape and gradient, were identified as the major governing parameters of soil erosion in the hilly and mountainous region. The net soil erosion rate over hillslope positions revealed highest at upper hillslope followed by ridge, middle and valley hillslope positions. The net soil erosion rate under the pine forest ranged from 8.0 to 14.6 t ha−1 yr−1, with an average rate of 9.9 t ha−1 yr−1. Erosion rate over the hillslope positions were found in accordance to the soil loss tolerance limit (SLTL) except for the upper hillslope, indicating it as critical slope position requires to adopt suitable conservation measures. The study signifies the role of the forest in mitigating soil erosion and, in turn, conserving soil resources. The findings provide crucial insights and guidance to land managers and decision-makers, emphasizing the necessity of conserving and restoring forests in the Himalayas.

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