Jingyi Ding

Dr. Jingyi Ding

orcid

Research Focus & Metrics

Academic Career Length

13Years (2014-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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1 December 2017 in Science of The Total Environment
Verified
Journal Article
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QFQiang Feng
Qiang Feng
Wenwu ZhaoWenwu Zhao
Wenwu Zhao
BFBojie Fu
Bojie Fu
JDJingyi Ding
Jingyi Ding
SWShuai Wang
Shuai Wang

12 August 2016 in Hydrology and Earth System Sciences
Verified
Journal Article
Open access
PDF file
XFXuening Fang
Xuening Fang
Wenwu ZhaoWenwu Zhao
Wenwu Zhao
LWLixin Wang
Lixin Wang
QFQiang Feng
Qiang Feng
JDJingyi Ding
Jingyi Ding
XZXiao Zhang
Xiao Zhang
Soil moisture in deep soil layers is a relatively stable water resource for vegetation growth in the semi-arid Loess Plateau of China. Characterizing the variations in deep soil moisture and its influencing factors at a moderate watershed scale is important to ensure the sustainability of vegetation restoration efforts. In this study, we focus on analyzing the variations and factors that influence the deep soil moisture (DSM) in 80–500 cm soil layers based on a soil moisture survey of the Ansai watershed in Yan'an in Shanxi Province. Our results can be divided into four main findings. (1) At the watershed scale, higher variations in the DSM occurred at 120–140 and 480–500 cm in the vertical direction. At the comparable depths, the variation in the DSM under native vegetation was much lower than that in human-managed vegetation and introduced vegetation. (2) The DSM in native vegetation and human-managed vegetation was significantly higher than that in introduced vegetation, and different degrees of soil desiccation occurred under all the introduced vegetation types. Caragana korshinskii and black locust caused the most serious desiccation. (3) Taking the DSM conditions of native vegetation as a reference, the DSM in this watershed could be divided into three layers: (i) a rainfall transpiration layer (80–220 cm); (ii) a transition layer (220–400 cm); and (iii) a stable layer (400–500 cm). (4) The factors influencing DSM at the watershed scale varied with vegetation types. The main local controls of the DSM variations were the soil particle composition and mean annual rainfall; human agricultural management measures can alter the soil bulk density, which contributes to higher DSM in farmland and apple orchards. The plant growth conditions, planting density, and litter water holding capacity of introduced vegetation showed significant relationships with the DSM. The results of this study are of practical significance for vegetation restoration strategies, especially for the choice of vegetation types, planting zones, and proper human management measures.

1 May 2023 in Nature Geoscience
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Journal Article
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DEDavid J. Eldridge
David J. Eldridge
Emilio GuiradoEmilio Guirado
Emilio Guirado
PRPeter B. Reich
Peter B. Reich
Raúl Ochoa-HuesoRaúl Ochoa-Hueso
Raúl Ochoa-Hueso
MVMiguel Berdugo Vega
Miguel Berdugo Vega
MDManuel Delgado-Baquerizo
Manuel Delgado-Baquerizo


12 April 2024 in Nature Plants
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Journal Article
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DEDavid J. Eldridge
David J. Eldridge
JDJingyi Ding
Jingyi Ding
JDJosh Dorrough
Josh Dorrough
MDManuel Delgado-Baquerizo
Manuel Delgado-Baquerizo
OSOsvaldo Sala
Osvaldo Sala
FMFernando T. Maestre
Fernando T. Maestre

21 December 2022 in Nature Plants
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Journal Article
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JDJingyi Ding
Jingyi Ding
DEDavid Eldridge
David Eldridge