EAPSI: Investigating the role of soil hydrophobicity on groundwater recharge beneath differing land uses in China's Loess Plateau

EAPSI：研究中国黄土高原不同土地利用下土壤疏水性对地下水补给的作用

• 批准号: 1415035
• 负责人: Zablon Adane
• 金额: $ 0.51万
• 依托单位: Adane Zablon A
• 依托单位国家: 美国
• 项目类别: Fellowship Award
• 财政年份: 2014
• 资助国家: 美国
• 起止时间: 2014-06-01 至 2015-05-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1415035&HistoricalAwards=false
• 关键词: EAPSI; Investigating; role; soil; hydrophobicity

Previous studies in the Loess Plateau have found that tree and shrub plantations have reduced groundwater recharge in the Loess Plateau. Whereas these studies have assumed that the reduced recharge is solely due to higher transpiration and rainfall interception, other studies suggested a link between soil hydrophobicity and reduced infiltration and recharge beneath plantations in the northern High Plains region of the United States that may also be applicable in China's Loess Plateau. In collaboration with Dr. Zhonge Pang and Dr. Tianming Huang at the Institute of Geology and Geophysics, this project aims to investigate hydrophobicity of near-surface sediments beneath differing land uses in order to determine the role of hydrophobicity on reduced recharge in the Loess Plateau. Further, the study will help determine whether plantation induced soil hydrophobicity is a phenomenon unique to the High Plains region.The proposed methods include new and traditional approaches including surface infiltration tests, ethanol water drop penetration tests on sediments up to 50 cm profile depth with 5 cm depth intervals, and water retention curves to determine soil hydraulic parameters. Leveraging detailed recharge studies that have already taken place, this project will examine patterns amongst hydrophobic soils, plantation types, and recharge rates from previously-observed data. In addition, the proposed study will determine the extent of soil hydrophobicity in each land use plot as a function of soil moisture content, organic carbon content, and profile depth. This NSF EAPSI award is funded in collaboration with the Chinese Ministry of Science and Technology.

以往在黄土高原的研究发现，乔灌木人工林减少了黄土高原地下水的补给。尽管这些研究假设补给减少仅仅是由于较高的蒸腾作用和降雨截留，但其他研究表明，土壤疏水性与美国北方高平原地区种植园下的渗透和补给减少之间存在联系，这也可能适用于中国的黄土高原。该项目与地质与地球物理研究所的庞忠革博士和黄天明博士合作，旨在研究不同土地利用下近地表沉积物的疏水性，以确定疏水性对黄土高原补给减少的作用。此外，这项研究将有助于确定是否种植园引起的土壤疏水性是一种独特的现象，高平原region.The建议的方法包括新的和传统的方法，包括表面入渗试验，乙醇水滴渗透试验的沉积物高达50厘米的剖面深度与5厘米的深度间隔，和水分保持曲线，以确定土壤水力参数。利用已经进行的详细的补给研究，该项目将根据以前观察到的数据，研究疏水性土壤、种植园类型和补给率之间的模式。此外，拟议的研究将确定土壤疏水性的程度，在每个土地利用地块作为土壤水分含量，有机碳含量和剖面深度的函数。NSF EAPSI奖是与中国科技部合作资助的。