師資
匡星星畢業(yè)于中國地質(zhì)大學(xué)(北京)，香港大學(xué)博士(水文地質(zhì))。在香港大學(xué)工作4年。現(xiàn)任南方科技大學(xué)環(huán)境科學(xué)與工程學(xué)院副教授（研究員）。主要研究方向?yàn)轱柡?非飽和流、水氣二相流、溶質(zhì)運(yùn)移數(shù)值模擬、以及地下水對(duì)氣候變化的響應(yīng)。在水資源領(lǐng)域頂級(jí)或重要學(xué)術(shù)期刊上發(fā)表論文20多篇。長期擔(dān)任水資源領(lǐng)域多個(gè)學(xué)術(shù)期刊的審稿人，包括Water Resources Research, Earth and Planetary Science Letters，Geophysical Research Letters，Groundwater，Vadose Zone Journal等?，F(xiàn)任國際水資源領(lǐng)域重要期刊Hydrogeology Journal副主編。2014年獲得AXA研究基金博士后獎(jiǎng)學(xué)金。
目前任職
南方科技大學(xué)環(huán)境科學(xué)與工程學(xué)院，副教授（研究員）
教育背景
2008-2012：博士(水文地質(zhì))，香港大學(xué)
2007-2008：碩士(水文學(xué)及水資源)，中國地質(zhì)大學(xué)(北京)
2003-2007：學(xué)士(水文與水資源工程)，中國地質(zhì)大學(xué)(北京)
工作經(jīng)歷
2017.04-至今：南方科技大學(xué)環(huán)境科學(xué)與工程學(xué)院，副教授（研究員）
2016-2017.04：南方科技大學(xué)環(huán)境科學(xué)與工程學(xué)院，助理教授
2014-2016：香港大學(xué)地球科學(xué)系，AXA博士后
2013-2014：香港大學(xué)地球科學(xué)系，博士后
2012-2013：香港大學(xué)地球科學(xué)系，研究助理
獲獎(jiǎng)情況及榮譽(yù)
2014：AXA研究基金博士后獎(jiǎng)學(xué)金
2007：北京市優(yōu)秀畢業(yè)生
2007：中國地質(zhì)大學(xué)(北京)優(yōu)秀畢業(yè)生
2005：中國石化獎(jiǎng)學(xué)金
2004：國家二等獎(jiǎng)學(xué)金
學(xué)術(shù)兼職
2014-至今：國際學(xué)術(shù)刊物《Hydrogeology Journal》副主編
研究領(lǐng)域
1) 飽和-非飽和流與水氣二相流參數(shù)模型研究
2) 飽和-非飽和流與水氣二相流試驗(yàn)與數(shù)值模擬
3) 多孔介質(zhì)溶質(zhì)運(yùn)移數(shù)值模擬
4) 地下水對(duì)氣候變化的響應(yīng)
簡要介紹
1) 飽和-非飽和流與水氣二相流參數(shù)模型研究
非飽和滲透系數(shù)是含水層中飽和-非飽和流與水氣二相流的關(guān)鍵參數(shù)。已有的非飽和滲透系數(shù)模型，對(duì)于飽和-非飽和流低估了實(shí)測(cè)值；對(duì)于水氣二相流則高估了實(shí)測(cè)值。不準(zhǔn)確的非飽和滲透系數(shù)可能是制約數(shù)值模擬精度的瓶頸?？镄切菆F(tuán)隊(duì)改進(jìn)了van Genuchten模型，新模型改進(jìn)了非飽和滲透系數(shù)對(duì)實(shí)測(cè)數(shù)據(jù)的吻合程度。成果發(fā)表在國際土壤學(xué)重要期刊《European Journal of Soil Science》。匡星星團(tuán)隊(duì)推導(dǎo)出了一個(gè)新的非飽和空氣滲透系數(shù)模型，提高了計(jì)算值與實(shí)測(cè)值之間的吻合程度。成果發(fā)表在國際水文水資源頂級(jí)期刊《Water Resources Research》。
滲透系數(shù)是控制地殼中流體流動(dòng)的最重要的參數(shù)。地殼的滲透系數(shù)隨深度衰減。已有的描述這種衰減關(guān)系的模型要么在地表數(shù)值趨于無窮大，要么隨深度衰減得太快。匡星星團(tuán)隊(duì)提出了一個(gè)新的模型，該模型克服了現(xiàn)有模型的缺點(diǎn)，可用于描述整個(gè)地殼的滲透系數(shù)隨深度的變化。成果發(fā)表在國際地球科學(xué)綜合重要期刊《Geophysical Research Letters》。
2) 飽和-非飽和流與水氣二相流試驗(yàn)與數(shù)值模擬
試驗(yàn)研究和數(shù)值模擬是研究地下水資源、地下水水質(zhì)的不可或缺的重要手段。上覆低滲透性地層的二元結(jié)構(gòu)潛水含水層在自然界普遍存在。研究這種二元結(jié)構(gòu)潛水含水層抽水試驗(yàn)引起的水、氣流動(dòng)機(jī)理以及空氣流對(duì)抽水試驗(yàn)的影響變得非常重要。匡星星團(tuán)隊(duì)通過室內(nèi)試驗(yàn)研究與數(shù)值模擬，從機(jī)理上闡明了這種二元結(jié)構(gòu)潛水含水層抽水試驗(yàn)引起的水氣二相流機(jī)理，包括雙層砂柱排水試驗(yàn)與模擬、雙層砂箱抽水試驗(yàn)與模擬、以及雙層潛水含水層抽水試驗(yàn)數(shù)值模擬。相關(guān)成果發(fā)表在國際水資源著名期刊上，包括《Water Resources Research》、《Hydrological Processes》、以及《Hydrogeology Journal》。
3) 多孔介質(zhì)溶質(zhì)運(yùn)移數(shù)值模擬
三角洲地區(qū)的含水層系統(tǒng)往往呈現(xiàn)出多層的特征，含水層與弱透水層交替出現(xiàn)。由于三角洲地區(qū)在經(jīng)濟(jì)社會(huì)中的重要性，三角洲地層中的溶質(zhì)運(yùn)移過程是一個(gè)受到廣泛關(guān)注的問題。基于對(duì)二元結(jié)構(gòu)潛水含水層的研究，建立了一個(gè)考慮連續(xù)沉積過程的溶質(zhì)運(yùn)移模型，并將該模型運(yùn)用于模擬珠江三角洲含水層-弱透水層系統(tǒng)中氯離子和氫氧同位素的運(yùn)移機(jī)理。相關(guān)成果發(fā)表在國際水資源重要期刊《Hydrological Processes》和《Hydrogeology Journal》。
4) 地下水對(duì)氣候變化的響應(yīng)
由于全球氣候變暖，高海拔地區(qū)的冰川正在后退，凍土正在退化。作為水循環(huán)中至關(guān)重要的一環(huán)，地下水也正在受到氣候變暖的影響。由于高海拔地區(qū)往往是大江大河的源頭地區(qū)，因此，研究高海拔地區(qū)氣候變暖對(duì)地下水流系統(tǒng)的影響，具有重要的意義。匡星星團(tuán)隊(duì)正在研究全球氣候變暖引起的青藏高原冰雪融化對(duì)地下水流系統(tǒng)的影響。由于全球氣候變暖，青藏高原上的冰雪和冰川正在融化。這種冰雪的融化可能對(duì)地下水流系統(tǒng)產(chǎn)生重大的影響。相關(guān)成果發(fā)表在該領(lǐng)域重要期刊《Journal of Geophysical Research: Atmospheres》。
講授的本科生課程
(1) 水力學(xué)
(2) 水力學(xué)基礎(chǔ)實(shí)驗(yàn)
(3) 地球科學(xué)實(shí)習(xí)
發(fā)表論著
1. Luo, X., X. Kuang, J. J. Jiao, S. Liang, X. Zhang, and H. Li (2016), Evaluation of lacustrine groundwater discharge, hydrological partition, and nutrient budgets in a proglacial lake in Qinghai-Tibet Plateau: Using 222Rn and stable isotopes, Journal of Geophysical Research: Biogeosciences, submitted.
2. Kuang, X., J. J. Jiao, and Y. Wang (2016), Chloride as tracer of solute transport in the aquifer-aquitard system in the Pearl River Delta, China, Hydrogeology Journal, 24(5), 1121–1132.
3. Kuang, X., and J. J. Jiao (2016), Review on climate change on the Tibetan Plateau during the last half century, Journal of Geophysical Research: Atmospheres, 121(8), 3979–4007.
4. Jiao, J. J., X. Zhang, Y. Liu, and X. Kuang (2015), Increased water storage in the Qaidam Basin, the North Tibet Plateau from GRACE gravity data, PLoS ONE, 10(10), e0141442, doi:10.1371/journal.pone.0141442.
5. Liu, Y., X. Kuang, J. J. Jiao, and J. Li (2015), Numerical study of variable-density flow and transport in unsaturated-saturated porous media, Journal of Contaminant Hydrology, 182, 117–130.
6. Kuang, X., J. J. Jiao, and K. Liu (2015), Numerical studies of vertical Cl?, δ2H, and δ18O profiles in the aquifer-aquitard system in the Pearl River Delta, China, Hydrological Processes, 29(19), 4199–4209.
7. Jiao, J. J., L. Shi, X. Kuang, C. M. Lee, Wyss W.-S. Yim, and S. Yang (2015), Reconstructed chloride concentration profiles below the seabed in Hong Kong (China) and their implications for offshore groundwater resources, Hydrogeology Journal, 23(2), 277–286.
8. Kuang, X., and J. J. Jiao (2014), An integrated permeability-depth model for Earth’s crust, Geophysical Research Letters, 41(21), 7539–7545.
9. Kuang X., J. J. Jiao, K. Zhang, and D. Mao (2014), Air and water flows induced by pumping tests in unconfined aquifers with low-permeability zones, Hydrological Processes, 28(21), 5450–5464.
10. Kuang, X., and J. J. Jiao (2014), A new equation for the soil water retention curve, European Journal of Soil Science, 65(4), 584–593.
11. Kuang, X., J. J. Jiao, and H. Li (2013), Review on airflow in unsaturated zones induced by natural forcings, Water Resources Research, 49(10), 6137–6165.
12. Huang, H., J. Qian, X. Kuang, B. Chen, and L. Ma (2013), The influence of low-permeability cap on capillary pressure during pumping in unconfined aquifer, Journal of Hydrodynamics, 25(6), 867–870.
13. Dong, P., X. Wang, L. Wan, X. Kuang, and T. Chen (2013), Sand column experiments and modeling study on coupling between groundwater level change and air flow (in Chinese), Earth Science - Journal of China University of Geosciences, 38(S1), 126–132.
14. Kuang, X., J. J. Jiao, H. Huang, and J. Qian (2013), Air and water flows in a large sand box with a two layer aquifer system, Hydrogeology Journal, 21(5), 977–985.
15. Wang, X.-S., J. J. Jiao, Y. Wang, J. A. Cherry, X. Kuang, K. Liu, C. Lee, and Z. Gong (2013), Accumulation and transport of ammonium in aquitards in the Pearl River Delta (China) in the last 10,000 years: conceptual and numerical models, Hydrogeology Journal, 21(5), 961–976.
16. Huang, H., J. Qian, X. Kuang, Z. Chen, and R. Li (2012), Experimental study of airflow induced by pumping tests in unconfined aquifer with low-permeability cap, Journal of Hydrodynamics, 24(4), 605–608.
17. Yang, L., X. Wang, J. J. Jiao, Y. Wang, and X. Kuang (2011), Identification of hydraulic parameters with slug test in clay soils (in Chinese), Geotechnical Investigation & Surveying, 39(6), 32–35.
18. Kuang, X., and J. J. Jiao (2011), A new model for predicting relative nonwetting phase permeability from soil water retention curves, Water Resources Research, 47, W08520, doi:10.1029/2011WR010728.
19. Kuang, X., J. J. Jiao, L. Wan, X. Wang, and D. Mao (2011), Air and water flows in a vertical sand column, Water Resources Research, 47, W04506, doi:10.1029/2009WR009030.
20. Chen, C., X. Kuang, and J. J. Jiao (2011), Reply to comments on “Methods to derive the differential equation of the free surface boundary”, Ground Water, 49(2), 142–143.
21. Chen, C., X. Kuang, and J. J. Jiao (2010), Reply to comments on “Methods to derive the differential equation of the free surface boundary”, Ground Water, 48(4), 490–493.
22. Chen, C., X. Kuang, and J. J. Jiao (2010), Methods to derive the differential equation of the free surface boundary, Ground Water, 48(3), 329–332.