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| 1 | Groundwater Systems and Resources in the Ordos Basin,China显示文摘Ordos 盆是在西北的中国的大规模沉积的盆。到顶的从底部的 hydrostratigraphic 单位是 pre 寒武纪的变形岩石,更低的古生代的碳酸盐岩石,上面对中生代碎屑状的岩石和新生代存款古生代。全部的厚度直到 6000 m。三个地下水系统在 Ordos 盆是在场的,基于地质的设置,即石灰岩地区常见的地形地下水系统,白垩纪碎屑状的地下水系统和第四级的地下水系统。这份报纸系统地描述每个系统的地下水流动模式和对地下水资源的全面评价。 | HOU Guangcai LIANG Yongping SU Xiaosi ZHAO Zhenghong TAO Zhengping YIN Lihe YANG Yuncheng WANG Xiaoyong | 2008 | Acta Geologica Sinica(English Edition)2008，82，5： | 5 |
| 2 | Growth and optical properties of ytterbium and rare earth ions codoped CaF2-SrF2 eutectic solid-solution(RE=Y^(3+),Gd^(3+),La^(3+))显示文摘Ytterbium and rare earth ions(RE=Y,Gd,La)codoped CaF_(2)-SrF_(2)single crystals(3 at%Yb,6 at%RE:CaF_(2)-SrF_(2))were fabricated by temperature gradient technology(TGT).All the space groups remain the same Fm3m as that of Yb:CaF_(2)-SrF_(2).The lattice parameter a,unit cell volume V,as well as bond length of Ca/Sr-F and F-F increase in the sequence of rare-earth ions radius Y^(3+) | Binbin Jiang Lihe Zheng Dapeng Jiang Handi Yin Jiangang Zheng Qiuhong Yang Guofeng Cheng Liangbi Su | 2021 | Journal of Rare Earths2021，39，4： | 2 |
| 3 | Quantification of groundwater recharge and evapotranspiration along a semi-arid wetland transect using diurnal water table fluctuations显示文摘Groundwater is a vital water resource in arid and semi-arid areas.Diurnal groundwater table fluctuations are widely used to quantify rainfall recharge and groundwater evapotranspiration(ET_(g)).To assess groundwater resources for sustainable use,we estimated groundwater recharge and ET_(g) using the diurnal water table fluctuations at three sites along a section with different depths to water table(DWT)within a wetland of the Mukai Lake in the Ordos Plateau,Northwest China.The water table level was monitored at an hourly resolution using a Keller DCX-22 A data logger that measured both the total pressure and barometric pressure,so that the effect of barometric pressure could be removed.At this study site,a rapid water table response to rainfall was observed in two shallow wells(i.e.,Obs1 and Obs2),at which diurnal water table fluctuations were also observed over the study period during rainless days,indicating that the main factors influencing water table variation are rainfall and ET_(g).However,at the deep-water table site(Obs3),the groundwater level only reacted to the heaviest rainfalls and showed no diurnal variations.Groundwater recharge and ET_(g) were quantified for the entire hydrological year(June 2017–June 2018)using the water table fluctuation method and the Loheide method,respectively,with depth-dependent specific yields.The results show that the total annual groundwater recharge was approximately 207 mm,accounting for 52%of rainfall at Obs1,while groundwater recharge was approximately 250 and 21 mm at Obs2 and Obs3,accounting for 63%and 5%of rainfall,respectively.In addition,the rates of groundwater recharge were mainly determined by rainfall intensity and DWT.The daily mean ET_(g) at Obs1 and Obs2 over the study period was 4.3 and 2.5 mm,respectively,and the main determining factors were DWT and net radiation. | JIA Wuhui YIN Lihe ZHANG Maosheng ZHANG Xinxin ZHANG Jun TANG Xiaoping DONG Jiaqiu | 2021 | Journal of Arid Land2021，13，5： | 1 |
| 4 | A GIS-based DRASTIC model for assessing groundwater vulnerability in the Ordos Plateau, China 显示文摘 | Yin Lihe Zhang Eryong Wang Xiaoyong | 2013 | Environmental Earth Sciences2013，69，： | 1 |
| 5 | Comparison and modifi- cation of methods for estimating evapotranspiration using diurnal groundwater level fluctuations in arid and semiarid regions 显示文摘 | YIN Lihe ZHOU Yangxiao GE Shemin | 2013 | Jour- nal of Hydrnlogy2013，496，24： | 1 |
| 6 | Dynamics of Interaction of Groundwater and Qigai Lake显示文摘Study on groundwater and surface water inter-actions is vital to the effective water resources management and aquatic eco-rehabilitation.In this study,measurements of water table and lake stage were conducted in Oigai Lake to study the interaction between groundwater and lake water.Hydrochemical data was also used as an alternative indicator to study the recharge-discharge functions of Qigai lake and groundwater.The study shows that there are two water-table configurations.In the configuration 1, | Lihe Yin Xi’an Center of Geological Survey,Xi’an 710054,China. | 2009 | 地学前缘2009，16，S1： | 0 |
| 7 | Using a Particle Tracking Method to Quantify Groundwater Circulation rates: a Case Study in the Ordos Plateau显示文摘Groundwater is a valuable resource in many areas, and commonly plays a key role in economic development. Therefore, groundwater circulation rates at different depths are key issues for groundwater development and management in the Ordos Plateau. In this study, a particle tracking method was used to quantify circulation rates in the Ordos plateau. The results show that groundwater mainly circulates in shallow groundwater systems up to 400m depth. The results of this study can be used to develop effective programs for groundwater management and development.. | Lihe Yin Hongyun Ma Jiaqiu Dong Xiaoyong Wang Ying Li | 2013 | Journal of Groundwater Science and Engineering2013，1，1： | 0 |
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