人物經歷
本科(2000-2004):水文與水資源工程,蘭州大學;
碩士(2004-2007):水文學及水資源,蘭州大學;
博士(2008-2010):水文地質,中國科學院地質與地球物理研究所;
博士後(2010-2012):中國科學院地質與地球物理研究所;
副研究員(2013.1.至今):中國科學院地質與地球物理研究所。
研究方向
乾旱半乾旱地區地下水補給與演化
地下水同位素示蹤與年代學
包氣帶-飽和帶污染物遷移轉化
深部地質工程地下水環境效應
主要貢獻
以第一作者發表SCI論文15篇,被SCI引用210餘次。擴展了乾旱半乾旱地區包氣帶溶質剖面的套用範圍,將其用於恢復地下水補給歷史、確定地下水補給機制和評價植被變化對地下水補給影響,並(1)發現了乾旱半乾旱地區普遍存在現今淺表水文過程與地下水不平衡現象,強調了包氣帶剖面在評價現代補給量及其變化中的作用;(2)確定了黃土塬區降水入滲補給以活塞流為主,地下水年齡在幾百到上萬年;(3)提出了基於包氣帶溶質剖面評價植被變化對地下水補給影響的定量化方法(ECMB)。在同位素水文學技術方法方面,提出利用氘盈餘確定水體鹽化機理的方法;基於多種環境示蹤技術建立了頁岩氣開發的地下水污染示蹤方法。
承擔科研項目
國家自然科學基金常規面上項目,編號:41877207
中國科學院戰略性先導科技專項子課題,編號:XDB10030603
國家自然科學基金常規面上項目,編號:41672254
國家自然科學基金青年基金項目,編號:41202183
中國博士後科學基金特別資助項目,編號:2012T50136
中國博士後科學基金面上資助項目,編號:20110490581
國家/部委重點實驗室開放基金項目
中國地質科學院礦產資源研究所項目
代表論著
Huang T, Fan Y, Long Y, Pang Z (2019) Quantitative calculation for the contribution of acid rain to carbonate weathering. Journal of Hydrology 568: 360–371 [link]
Huang T, Pang Z, Liu J, Ma J, Gates J (2017) Groundwater recharge mechanism in an integrated tableland of the Loess Plateau, northern China: insights from environmental tracers. Hydrogeology Journal 25(7): 2049–2065 [link]
Huang T, Pang Z, Liu J, Yin L, Edmunds WM (2017) Groundwater recharge in an arid grassland as indicated by soil chloride profile and multiple tracers. Hydrological Processes 31(5): 1047-1057 [link]
Huang T, Pang Z, Li J, Xiang Y, Zhao Z(2017) Mapping groundwater renewability using age data in the Baiyang alluvial fan, NW China. Hydrogeology Journal 25(3): 743-755 [link]
Huang T, Pang Z, Tian J, Li Y, Yang S, Luo L (2017) Methane content and isotopic composition of shallow groundwater: implications for environmental monitoring related to shale gas exploitation. Journal of Radioanalytical and Nuclear Chemistry 312(3):577-585 [link]
Huang T, Hao Y, Pang Z, Li Z, Yang S (2017) Radioactivity of soil, rock and water in a shale gas exploitation area, SW China. Water 9(5), 299, doi: 10.3390/w9050299 [link]
Huang T, Yang S, Liu J, Li Z (2016) How much information can soil solute profiles reveal about groundwater recharge? Geosciences Journal 20: 495-502. [link]
Huang T, Pang Z, Edmunds WM (2013) Soil profile evolution following land-use change: implications for groundwater quantity and quality. Hydrological Processes 27: 1238-1252 [link]
Huang T, Pang Z, Yuan L (2013) Nitrate in groundwater and the unsaturated zone in (semi)arid northern China: baseline and factors controlling its transport and fate. Environmental Earth Sciences 70: 145-156 [link]
Huang T, Pang Z, Chen Y, Kong Y (2013) Groundwater circulation relative to water quality and vegetation in an arid transitional zone linking oasis, desert and river. Chinese Science Bulletin 58: 3088-3097[link]
Huang T, Pang Z (2012) The role of deuterium excess in determining the water salinisation mechanism: a case study of the arid Tarim River Basin, NW China. Applied Geochemistry 27: 2382-2388 [link]
Huang T, Pang Z (2011) Estimating groundwater recharge following land-use change using chloride mass balance of soil profiles: a case study at Guyuan and Xifeng in the Loess Plateau of China. Hydrogeology Journal 19: 177-186 [link]
Huang T, Pang Z (2010) Changes in groundwater induced by water diversion in the Lower Tarim River, Xinjiang Uygur, NW China: evidence from environmental isotopes and water chemistry. Journal of Hydrology 387: 188-201 [link].
獲獎記錄
中國科學院青年創新促進會會員
中國自然資源學會青年科技獎
國際水岩相互作用(WRI)GMZ Scholarship
甘肅省水利科技進步一等獎