[1] 张兵,宋献方,张应华,等.第二松花江流域地表水与地下水相互关系[J].水科学进展,2014,25(3):336-347. [2] 杨智.鄂尔多斯高原海流兔河地下水和地表水交互作用关系研究[D].北京:中国地质大学,2014. [3] Sarkar A,Shekhar S.The controls on spatial and temporal variation of hydrochemical facies and major ion chemistry in groundwater of South West District,Delhi,India[J].Environmental Earth Sciences,2015,74(12):7783-7791. [4] Herojeet R,Rishi M S,Lata R,et al.Application of environmetrics statistical models and water quality index for groundwater quality characterization of alluvial aquifer of Nalagarh Valley,Himachal Pradesh,India[J].Sustainable Water Resources Management,2016,2(1):39-53. [5] Pierret M C,Stille P,Prunier J,et al.Chemical and U-Sr isotopic variations in stream and source waters of the Strengbach watershed (Vosges mountains,France)[J].Hydrology & Earth System Sciences,2014,18(10):3969-3985. [6] Nigro A,Sappa G,Barbieri M.Application of boron and tritium isotopes for tracing landfill contamination in groundwater[J].Journal of Geochemical Exploration,2016,172:101-108. [7] Gómez E,Barmen G,Rosberg J E.Groundwater origins and circulation patterns based on isotopes in challapampa aquifer,Bolivia[J].Water,2016,8(5):207. [8] Hiatt M,Passalacqua P.Hydrological connectivity in river deltas:the first-order importance of channel-island exchange[J].Water Resources Research,2015,51(4):2264-2282. [9] Rugel K,Golladay S W,Jackson C R,et al.Delineating groundwater/surface water interaction in a karst watershed:Lower Flint River Basin,southwestern Georgia,USA[J].Journal of Hydrology Regional Studies,2016,5(5):1-19. [10] Anibas C,Schneidewind U,Vandersteen G,et al.From streambed temperature measurements to spatial-temporal flux quantification:using the LPML method to study groundwater-surface water interaction[J].Hydrological Processes,2016,30(2):203-216. [11] 詹泸成,陈建生,张时音.洞庭湖湖区降水-地表水-地下水同位素特征[J].水科学进展,2014,25(3):327-335. [12] 姜海宁,谷洪彪,迟宝明,等.新疆昭苏-特克斯盆地地表水与地下水转化关系研究[J].干旱区地理,2016,39(5):1078-1088. [13] 磴口县人民政府.城市建设[EB/OL].[2017-06-09].http://www.nmgdk.gov.cn/dkbxgk/dkcsjs/. [14] 李梦,雷敏,杨海娟.基于EMD西安市虚拟水总量波动及其成因的时空多尺度分析[J].干旱区地理,2017,40(2):469-476. [15] Hu W,Biswas A,Si B C.Application of multivariate empirical mode decomposition for revealing scale-and season-specific time stability of soil water storage[J].Catena,2014,113(1):377-385. [16] 李合龙,王龙,李明建,等.基于平均包络线匹配算法的EMD端点效应分析及在股价趋势分解中的应用[J].系统工程理论与实践,2013,33(8):2072-2079. [17] 杨茂,陈郁林.基于EMD分解和集对分析的风电功率实时预测[J].电工技术学报,2016,31(21):86-93. [18] 于正军,董冬冬,宋维琪,等.相带控制下协克里金方法孔隙度预测[J].地球物理学进展,2012,27(4):1581-1587. [19] 高秀鹤,黄大年,孙思源,等.重力梯度数据协克里金三维反演确定岩脉倾向[J].吉林大学学报(地球科学版),2017,47(2):589-596. [20] 马欢,岳德鹏,Yang D,等.基于数据同化的地下水埋深插值研究[J].农业机械学报,2017,48(4):206-214. [21] 王宏伟,黄春林,侯金亮.一种融合遥感和地面观测资料的雪深空间插值方法[J].遥感技术与应用,2014,29(6):993-1000. [22] Li Z,Liu X,Ma T,et al.Retrieval of the surface evapotranspiration patterns in the alpine grassland-wetland ecosystem applying SEBAL model in the source region of the Yellow River,China[J].Ecological Modelling,2013,270(270):64-75. [23] 张志杰,杨树青,史海滨,等.内蒙古河套灌区灌溉入渗对地下水的补给规律及补给系数[J].农业工程学报,2011,27(3):61-66. [24] 顾慰祖,陆家驹,谢民,等.乌兰布和沙漠北部地下水资源的环境同位素探讨[J].水科学进展,2002,13(3):326-332. [25] 汪敬忠,吴敬禄,曾海鳌,等.内蒙古河套平原水体同位素及水化学特征[J].地球科学与环境学报,2013,35(4):104-112. [26] 费宇红,苗晋祥,张兆吉,等.华北平原地下水降落漏斗演变及主导因素分析[J].资源科学,2009,31(3):394-399. |