Volume 39, Issue 3 e70103
RESEARCH ARTICLE

Understanding Hydrological Process Change due to Re-Vegetation in a Mountainous Watershed of Northern China

Fan Zhou

Fan Zhou

College of Water Resources and Hydropower Engineering, North China Electric Power University, Beijing, People's Republic of China

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Shengping Wang

Corresponding Author

Shengping Wang

College of Water Resources and Hydropower Engineering, North China Electric Power University, Beijing, People's Republic of China

Correspondence:

Shengping Wang ([email protected])

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Siyi Qu

Siyi Qu

College of Water Resources and Hydropower Engineering, North China Electric Power University, Beijing, People's Republic of China

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Wenxin Li

Wenxin Li

College of Water Resources and Hydropower Engineering, North China Electric Power University, Beijing, People's Republic of China

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Desheng Cai

Desheng Cai

College of Water Resources and Hydropower Engineering, North China Electric Power University, Beijing, People's Republic of China

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Qingfeng Hai

Qingfeng Hai

College of Water Resources and Hydropower Engineering, North China Electric Power University, Beijing, People's Republic of China

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Mengyao Ma

Mengyao Ma

College of Water Resources and Hydropower Engineering, North China Electric Power University, Beijing, People's Republic of China

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Peter Strauss

Peter Strauss

Institute for Land and Water Management Research, Federal Agency for Water Management, Petzenkirchen, Austria

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Zhiwei Wang

Zhiwei Wang

Forestry and Grassland Office of Weichang County, Chengde, Hebei, People's Republic of China

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Yi Ren

Yi Ren

Forestry and Grassland Office of Weichang County, Chengde, Hebei, People's Republic of China

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Liping Zhang

Liping Zhang

Forestry and Grassland Office of Weichang County, Chengde, Hebei, People's Republic of China

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First published: 11 March 2025

Funding: The National Key Research and Development Program of China (Grant Number: 2022YFF1302501-02).

ABSTRACT

Hydrological processes of mountainous watersheds commonly impact water resource supply in downstream areas. To better understand how re-vegetation affects the different hydrological pathways of watersheds, we investigated their change at various temporal scales for the Xiaoluan River watershed, a typical meso-scale watershed featuring a plateau–mountain transition topography in northern China. For the non-growing season from 2006 to 2020, the groundwater discharge of the watershed and the wetting of the watershed in terms of the Horton Index significantly increased, and the recession process in terms of the recession coefficient (k) was considerably prolonged. We suggest that re-vegetation and snowmelt were responsible for this change, but they affected the hydrological processes differently. That is, re-vegetation might improve the water storage capacity of the shallow soil layers of the watershed, thereby enhancing the capacity of groundwater recharge and discharge. Meanwhile, snowmelt may provide available water for recharging and discharging the watershed. Because reforestation progresses and global climate change continues, more complex hydrological processes are to be expected. Therefore, continuous monitoring and detailed investigations of subsurface hydrological processes will be necessary for adaptive watershed management.

Data Availability Statement

Research data are not shared.

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