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[1]WANG Leiqin,WANG Fei,LI Pengfei.Relationships Between Vegetation Restoration and Soil Moisture on the Loess Plateau[J].Research of Soil and Water Conservation,2017,24(06):179-185,193.

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Relationships Between Vegetation Restoration and Soil Moisture on the Loess Plateau

Research of Soil and Water Conservation[ISSN 1005-3409/CN 61-1272/P] Volume: 24 Number of periods: 2017 06 Page number: 179-185,193 Column: Public date: 2017-11-24

Title:: Relationships Between Vegetation Restoration and Soil Moisture on the Loess Plateau

Author(s):: WANG Leiqin¹, WANG Fei^1,2, LI Pengfei²; 1. Institute of Soil and Water Conservation, Northwest A & F University, Yangling, Shaanxi 712100, China;
2. Institute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Water Resources, Yangling, Shaanxi 712100, China

Keywords:: Loess Plateau; vegetation restoration; similar precipitation condition; NDVI; SWI; remote sensing

CLC:: S152.7

DOI:: -

Abstract:: On the Loess Plateau, soil moisture is one of the major factors impacting the sustainability of vegetation restoration. In this study, we used datasets on precipitation, vegetation cover and soil moisture content to investigate the changing trends and regional variabilities of vegetation cover and soil moisture across the Loess Plateau between 1992 and 2013 at a 25 km scale. The results showed that:(1) vegetation cover for most areas of the Loess Plateau experienced a significant increasing trend, while soil moisture for majority parts of the plateau underwent an insignificant change; (2) under the similar precipitation condition, there were mainly two types of vegetation cover-soil moisture changes, which were increased vegetation coverage and soil moisture and increased vegetation coverage and decreased soil moisture. Regional variabilities of changes in vegetation cover and soil moisture were large, further studies were desirable to understand the relationship between vegetation restoration and soil moisture changes, and therefore to improve the sustainability of vegetation restoration on the Loess Plateau.

References:: [1] 李玉山.黄土区土壤水资源循环特征及其对陆地水文循环的影响[J].生态学报,1983,3(2):91-101.
[2] 穆兴民.试论黄土高原土壤水资源的地带性与非地带性[J].土壤学报,1999,36(2):237-244.
[3] 杨朝瀚.黄土丘陵沟壑区几种主要水土保持型植被水分生态特征研究[D].北京:中国林业科学研究院,2006.
[4] 王云强.黄土高原地区土壤干层的空间分布与影响因素[D].北京:中国科学院研究生院,2010.
[5] 张建军,李慧敏,徐佳佳.黄土高原水土保持林对土壤水分的影响[J].生态学报,2011,31(23):71-81.
[6] 徐学选,刘文兆,高鹏,等.黄土丘陵区土壤水分空间分布差异性探讨[J].生态环境,2003,12(1):52-55.
[7] 王孟本,李洪建,柴宝峰.极端降水条件对林地水分循环的影响[J].土壤侵蚀与水土保持学报,1996,2(3):83-87,92.
[8] 李锋瑞,赵松岭.陇东黄土旱塬不同降水年型作物土壤水分时空分异特征分析[J].兰州大学学报:自然科学版,1996,32(2):99-107.
[9] 李洪建,王孟本,柴宝峰.晋西北人工林土壤水分特点与降水关系研究[J].土壤侵蚀与水土保持学报,1998,4(4):60-65.
[10] Qiu Y, Fu B, Wang J, et al. Soil moisture variation in relation to topography and land use in a hillslope catchment of the Loess Plateau, China[J]. Journal of Hydrology, 2001,240:243-263.
[11] 王飞,穆兴民,李锐,等.相似性降水条件下北洛河水沙变化特征[J].水资源与水工程学报,2008,19(6):36-40.
[12] D’urso G, Minacapilli M. A semi-empirical approach for surface soil water content estimation from radar data without a-priori information on surface roughness[J]. Journal of Hydrology, 2006,321(1):297-310.
[13] 焦俏,王飞,李锐,等. ERS卫星反演数据在黄土高原近地表土壤水分中的应用研究[J].土壤学报,2014,51(6):1388-1397.
[14] 樊廷录.黄土高原旱作地区径流农业的研究[D].陕西杨凌:西北农林科技大学,2002.
[15] 王力.陕北黄土高原土壤水分亏缺状况与林木生长关系[D].陕西杨凌:西北农林科技大学,2002.
[16] 高海清.陕北地区退耕还林(草)可持续发展支撑体系研究[D].陕西杨凌:西北农林科技大学,2009.
[17] Mu L, Liang Y, Han R. Assessment of the soil organic carbon sink in a project for the conversion of farmland to forestland:A case study in Zichang County, Shaanxi, China[J]. PloS ONE, 2014,9(4):e94770.
[18] Chen Y, Wang K, Lin Y, et. al. Balancing green and grain trade[J]. Nature Geoscience, 2015,8(10):1-3.
[19] 王娟,卓静.基于RS和GIS的陕北黄土高原退耕还林区土壤侵蚀定量评价[J].水土保持通报,2015,35(1):220-223.
[20] 栾勇.退耕还林对黄土高原小流域土壤侵蚀控制效果研究[D].北京:北京林业大学,2008.
[21] 王志杰.延河流域植被与侵蚀产沙特征研究[D].北京:中国科学院研究生院(教育部水土保持与生态环境研究中心),2014.
[22] 陈浩,梁广林,周金星,等.黄河中游植被恢复对流域侵蚀产沙的影响与治理前景[J].中国科学D辑:地球科学,2005(5):452-463.
[23] Zribi M, PardéM, De Rosnay P, et al. ERS scatterometer surface soil moisture analysis of two sites in the south and north of the Sahel region of West Africa[J]. Journal of Hydrology, 2009,375(1):253-261.
[24] Scipal K. Global soil moisture retrieval from ERS scatterometer data[D]. Austria:Institute for Photogrammetry and Remote Sensing, Vienna University of Technology, 2002.
[25] Zhao D, Kuenzer C, Fu C, et al. Evaluation of the ERS scatterometer-derived soil water index to monitor water availability and precipitation distribution at three different scales in China[J]. Journal of Hydrometeorology, 2008,9(3):549-562.
[26] 蒋冲,王飞,穆兴民,等.土壤湿度指数在黄土高原的适宜性评价[J].灌溉排水学报,2012,31(3):31-36.
[27] Jiao Q, Li R, Wang F, et al. Impacts of re-vegetation on surface soil moisture over the Chinese Loess Plateau based on remote sensing datasets[J]. Remote Sensing, 2016,8(2):156.
[28] 杨荣金,傅伯杰,刘国华,等.黄土丘陵沟壑区生态环境建设中的水问题:以延河流域为例[J].环境科学,2004,25:37-42.
[29] 穆兴民.黄土高原人工林对区域深层土壤水环境的影响[J].土壤学报,2003,40(2):210-217.
[30] 马长炯,马宁,史世斌.内蒙古后套绿洲水资源合理利用[J].干旱区资源与环境,1995,9(3):113-121.
[31] 李鹏飞.植被恢复对黑岱沟煤矿排土场土壤性质和质量的影响研究[D].陕西杨凌:西北农林科技大学,2014.
[32] 陈怡平,骆世明,李凤民,等.对延安黄土沟壑区农业可持续发展的建议[J].地球环境学报,2015,6(5):265-269.
[33] Liu Q, Yang Z, Cui B. Spatial and temporal variability of annual precipitation during 1961-2006 in Yellow River Basin, China[J]. Journal of Hydrology, 2008,361(3):330-338.
[34] 杨文治.黄土高原土壤水资源与植树造林[J].自然资源学报,2001,16(5):433-438.
[35] 李振朝.近50年黄土高原气候变化特征分析[J].干旱区资源与环境,2008,22(3):57-62.
[36] 付东磊,刘梦云,刘林,等.黄土高原不同土壤类型有机碳密度与储量特征[J].干旱区研究,2014,31(1):44-50.
[37] 李玉山,韩仕峰,汪正华.黄土高原土壤水分性质及其分区[J].中国科学院西北水土保持研究所集刊,1985(2):1-17.

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