Effect of vegetation restoration type and topography on soil water storage and infiltration capacity in the Loess Plateau, China

被引:10
|
作者
Qiu, Dexun
Xu, Ruirui
Gao, Peng
Mu, Xingmin
机构
[1] Northwest A&F Univ, Inst Soil & Water Conservat, State Key Lab Soil Eros & Dryland Farming Loess P, Yangling 712100, Shaanxi, Peoples R China
[2] Chinese Acad Sci, Inst Soil & Water Conservat, State Key Lab Soil Eros & Dryland Farming Loess P, Yangling 712100, Shaanxi, Peoples R China
[3] Minist Water Resources, Yangling 712100, Shaanxi, Peoples R China
[4] Univ Chinese Acad Sci, Beijing 100049, Peoples R China
基金
中国国家自然科学基金;
关键词
Vegetation restoration; Soil water content; Soil water storage; Soil infiltration; Slope position; Loess Plateau; DIFFERENT LAND USES; HYDRAULIC-PROPERTIES; PREFERENTIAL FLOW; SLOPE POSITION; MOISTURE; AFFORESTATION; CATCHMENT; STABILITY; INFILTRABILITY; VARIABILITY;
D O I
10.1016/j.catena.2024.108079
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Vegetation restoration effectively mitigates soil erosion and improves soil properties, but in drylands, it can lead to soil water scarcity and disrupt ecological balance. Until now, limited research has examined the combined effects of vegetation restoration type and topography on soil water and infiltration in the Loess Plateau of China. Here, we investigated soil water content (SWC), soil water storage (SWS), soil infiltration rates and related soil properties in typical forestland, shrubland, and grassland across five slope positions on steep slopes, and compared them with cropland. The results indicated that vegetation restoration significantly decreased SWS compared to cropland. Across the entire 0 - 500 cm depth, reductions were observed at 30.9 %, 33.2 %, and 20.8 % for forestland, shrubland, and grassland, respectively, with forestland and shrubland demonstrating a more pronounced decrease, particularly in deeper soil layers. Shrubland had the lowest SWS on the upper, middle, and top slopes, while forestland showed the lowest SWS on the lower and foot slopes. In terms of infiltration, vegetation restoration generally increased steady infiltration rate but resulted in reduced initial and mean infiltration rates (except for shrubland). Shrubland had the highest infiltration rates, followed by forestland, while grassland had the lowest rates. Soil infiltration rates decreased gradually along the slope, indicating that the impact of vegetation restoration on soil infiltration improvement weakened with lower slope positions. Vegetation restoration type had a stronger direct and total effects on infiltration than slope position. Yet, the indirect influence of slope position through clay content and SWC outweighed that of vegetation restoration type. Our findings highlight the comprehensive assessment of the eco-hydrological effects of vegetation restoration is essential for identifying suitable species and designing optimal spatial distribution, ultimately maximizing the ecological benefits of the restoration. These insights can offer valuable guidance for ecological restoration and land management in fragile dryland ecosystems.
引用
收藏
页数:11
相关论文
共 50 条
  • [31] Soil hydraulic conductivity as affected by vegetation restoration age on the Loess Plateau, China
    Ren Zongping
    Zhu Liangjun
    Wang Bing
    Cheng Shengdong
    JOURNAL OF ARID LAND, 2016, 8 (04) : 546 - 555
  • [32] Changes in soil properties across a chronosequence of vegetation restoration on the Loess Plateau of China
    Jiao, Feng
    Wen, Zhong-Ming
    An, Shao-Shan
    CATENA, 2011, 86 (02) : 110 - 116
  • [33] Soil hydraulic conductivity as affected by vegetation restoration age on the Loess Plateau, China
    Zongping Ren
    Liangjun Zhu
    Bing Wang
    Shengdong Cheng
    Journal of Arid Land, 2016, 8 : 546 - 555
  • [34] Soil hydraulic conductivity as affected by vegetation restoration age on the Loess Plateau,China
    REN Zongping
    ZHU Liangjun
    WANG Bing
    CHENG Shengdong
    JournalofAridLand, 2016, 8 (04) : 546 - 555
  • [35] Effects of microplastics on water infiltration in agricultural soil on the Loess Plateau, China
    Liu, Zihan
    Cai, Lu
    Dong, Qinge
    Zhao, Xiaoli
    Han, Jianqiao
    AGRICULTURAL WATER MANAGEMENT, 2022, 271
  • [36] Soil water storage capacity under chronosequence of revegetation in Yanhe watershed on the Loess Plateau, China
    Jiao, Feng
    Wen, Zhong-Ming
    An, Shao-Shan
    SPRINGERPLUS, 2013, 2
  • [37] Interaction of soil water storage and stoichiometrical characteristics in the long-term natural vegetation restoration on the Loess Plateau
    Zhang, Yong-wang
    Shangguan, Zhou-ping
    ECOLOGICAL ENGINEERING, 2018, 116 : 7 - 13
  • [38] Regional effects of vegetation restoration on water yield across the Loess Plateau, China
    Feng, X. M.
    Sun, G.
    Fu, B. J.
    Su, C. H.
    Liu, Y.
    Lamparski, H.
    HYDROLOGY AND EARTH SYSTEM SCIENCES, 2012, 16 (08) : 2617 - 2628
  • [39] Effects of vegetation restoration on soil physical properties of abandoned farmland on the Loess Plateau, China
    Jing Li
    Zhanbin Li
    Mengjing Guo
    Peng Li
    Shengdong Cheng
    Bo Yuan
    Environmental Earth Sciences, 2018, 77
  • [40] Soil infiltration rate of forestland and grassland over different vegetation restoration periods at Loess Plateau in northern hilly areas of China
    Kalhoro, Shahmir Ali
    Ding, Kang
    Zhang, Beiying
    Chen, Wenyuan
    Hua, Rui
    Shar, Akhtar Hussain
    Xu, Xuexuan
    LANDSCAPE AND ECOLOGICAL ENGINEERING, 2019, 15 (01) : 91 - 99