首页|应用改进的Morgan-Morgan-Finney模型评估土壤侵蚀易感性:以尼泊尔Kulekhani流域为例

应用改进的Morgan-Morgan-Finney模型评估土壤侵蚀易感性:以尼泊尔Kulekhani流域为例

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本研究旨在考察Kulekhani流域土地利用与土地覆盖(LULC)动态变化及土壤侵蚀情况,并对 2000 年至 2020 年不同LULC类别进行分析.研究结果显示,Kulekhani流域森林土地比例从 2000 年的 60.72%上升至 2010年的 62.43%,2020年达到64.75%.水域面积有小幅增加,2000年占比为 1.07%,2020年增加到 1.08%.相应地,荒地面积从 0.21%增至 0.35%.相反,农业用地比例逐渐减少,2000年为 38%,2010年为 36.24%,2020年降至 33.82%.使用改进的Morgan-Morgan-Finney模型估算土壤流失量显示,2000年到 2010年期间,加权平均土壤流失量呈下降趋势,而 2010年到 2020年期间略微增加.计算得出的土壤流失值分别为 2000年 8.64 t ha-1 yr-1、2010年 7.12 t ha-1 yr-1 和 2020年 7.30 t ha-1 yr-1.土壤侵蚀易感性图表明,2000年到 2020年期间,非常低风险的土壤侵蚀区域有所增加,主要集中在森林地区,而农业区域则显示出低到中度的易感性.此外,荒地区域显示出中高度的土壤侵蚀易感性.为解决这些问题,建议未来的努力应包括在荒地地区进行造林计划,在农业区域实施保护耕作方式,并采取适当的道路稳定措施.
Assessing Soil Erosion Susceptibility Using Revised Morgan-Morgan-Finney Model:A Case Study from Kulekhani Watershed,Makawanpur,Nepal
The research was conducted within the Kulekhani Watershed with the objective of examining changes in Land Use Land Cover(LULC)dynamics and soil erosion across various LULC categories spanning from 2000 to 2020.The findings regarding the LULC classification in the Kulekhani Watershed revealed a steady rise in forested land,escalating from 60.72%in 2000 to 62.43%in 2010,and ultimately reaching 64.75%of the total area by 2020.The extent of water bodies exhibited a marginal increase from 1.07%in 2000 to 1.08%in 2020.Correspondingly,barren land expanded from 0.21%to 0.26%,eventually reaching 0.35%over the successive time intervals.Con-versely,agricultural land dwindled over these periods,comprising 38%in 2000,36.24%in 2010,and ultimately de-clining to 33.82%by 2020.The utilization of the Revised Morgan-Morgan-Finney(RMMF)model for soil loss esti-mation demonstrated a declining trend in weighted average soil loss during the years 2000 to 2010,followed by a slight increase between 2010 and 2020.The calculated soil loss values were recorded as 8.64 t ha-1 yr-1,7.12 t ha-1 yr-1,and 7.30 t ha-1 yr-1 for the years 2000,2010,and 2020 respectively.Similarly,the erosion susceptibility map illustrated a rising pattern in the very low-risk soil erosion zone from 2000 to 2020,primarily prominent within for-ested regions,while exhibiting a low to moderate susceptibility in agricultural zones.Moreover,barren areas dis-played a moderate to high susceptibility to soil erosion.To address these concerns,future endeavors are recom-mended to encompass afforestation initiatives in barren regions,implement conservation farming practices in ag-ricultural areas,and adopt appropriate measures for road stabilization.

watersedimentland useland coversloperainfall

THAPA Rabin、JOSHI Rajeev、BHATTA Binod、GHIMIRE Santosh

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尼泊尔赫陀达农林大学林业学院,Hetauda 44107,尼泊尔

尼泊尔乌达布尔农林大学自然资源管理学院,Udayapur,Katari 56310,尼泊尔

泥沙 土地利用 土地覆盖 坡度 降雨量

2024

资源与生态学报(英文版)
中国科学院地理科学与资源研究所

资源与生态学报(英文版)

CSTPCD
影响因子:0.388
ISSN:1674-764X
年,卷(期):2024.15(1)
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