The distribution of Caledonian residuum reservoirs in the south of Ordos Basin is mainly controlled by karst palaeogeomorphology, strata of residuum and sedimentary facies.
鄂尔多斯盆地南部加里东期风化壳储集层的分布主要受岩溶古地貌、风化壳层位及沉积相控制。
There developed a vast area of weathering crust karst reservoirs on top Ordovician in Ordos Basin.
鄂尔多斯盆地在奥陶系顶部发育大面积的风化壳岩溶储层。
There are closer relations among pore groundwater system, Karst groundwater system and fissure groundwater system in Taiyuan basin.
太原盆地孔隙水与周边岩溶水、砂岩裂隙水有密切的水力联系。
There are many factors that affect the low flow in a karst basin, such as climate, catchment area, lithology, soil, landform and so on, most of which are uncertain.
喀斯特流域枯水径流特征值的影响因素很多，如气候、流域面积、岩性、土壤、地貌等等，而能够确知的信息不多。
The karst vugs in the fine dolomites of Ordovician in Ordos Basin are the result of long time action caused by deeply buried hot water karst.
鄂尔多斯盆地奥陶系深部白云岩中的溶蚀孔洞，其成因属于热水岩溶作用的结果。
This paper discusses the forming conditions of deep Karst groundwater in Sichuan basin and its surroundings. The cyclic pattern of deep Karst groundwater is summed up.
本文讨论了四川盆地及盆周地区深部岩溶地下水形成条件，对深部岩溶地下水的循环模式进行了归纳总结。
The city of Guiyang is located in a wide karst valley basin in the central part of Guizhou Plateau, where carbonaceous rocks are developing and karst groundwater sources are abundant.
贵阳市位于贵州高原中部的一个岩溶宽谷盆地中，岩溶地层发育，地下水资源丰富。
Xingwen Karst Geopark is located in Xingwen County, Yibin City, Sichuan Province, where it is a transitional zone between the Sichuan Basin and the Yunnan-Guizhou Plateau.
兴文喀斯特地质公园位于四川省宜宾市兴文县。这里也是四川盆地和云贵高原交界处。
Based on the analysis and study on the physical properties of karst soil in Guizhou Wujiang river basin in different type of vegetation and different degree of erosion.
本文分析研究了贵州乌江流域喀斯特土壤在不同植被类型和不同侵蚀程度条件下的土壤主要物理性质。
The karst groundwater system in Ordos basin consists of 22 sub-systems with various catchment sizes.
鄂尔多斯盆地周边岩溶分布区由22个汇水面积不等的岩溶地下水子系统组成。
In this paper the water balance method is used to analyse groundwater resources and allowable exploitation quantity of karst fissure water in the Mishian basin.
本文运用水均衡方法，对密县盆地地下岩溶水资源及允许开采量等进行了分析。
Liujiang basin is an important water source area of Qinhuangdao city. The surface collapse will happen at hidden karst areas, due to much exploiting of ground-water.
柳江盆地是秦皇岛市的重要水源地，由于大量开采地下水，在隐伏岩溶发育区将引起地表塌陷。
Abstract : The buried depth of karst paleo-caves in Tahe oilfield, Tarim basin is deeper than others throughout the world. But little is known about the reason why it did not collapse.
摘要 ：塔河油田奥陶系古岩溶洞穴埋藏深度之大在世界范围内罕见，但对其为何没有垮塌殆尽的原因却知之甚少。
The karst groundwater in this basin is controlled by the different type and scale of groundwater storing geological structures.
该盆地岩溶水受不同类型和规模的蓄水构造控制。
The groundwater in Karst spring basin has a characteristic of concentration drain, it is similar to unsteady orifice outflow in fluid mechanics.
岩溶泉域地下水具有集中排泄的特点，它类似于流体力学中的非恒定孔口出流。
The paper has treated the karst groundwater resources of the Sangu spring basin as research object, and six aspects have been researched.
本文在上述背景下对晋城市三姑泉域岩溶地下水资源进行了六个方面的研究。
The Wenshan basin is karst faulted basin, the main rock is carbonate, clay and clastic.
文山盆地属于岩溶断陷盆地，研究区基岩主要为碳酸盐岩、粘土岩与碎屑岩。
The Xijiang River's inorganic carbon source was major from karst process in the drainage basin. Due to the "washing effect" , the content of HCO3- ion increased in the wet season.
西江无机碳主要来源于岩溶作用，由于受河流冲刷效应影响，丰水期HCO_3~-离子含量升高；
Paleo-karst was developed in Ordovician limestones at the west of Lungu area in Tarim basin.
塔里木轮古西地区奥陶系灰岩是古岩溶发育的有利场所。
In Karst spring basin the groundwater resreve computation is a important task for Karst-water resource evaluation in this basin.
岩溶泉域地下水储量的计算是该区域岩溶水资源评价的一项重要任务。
The influence factors of low water based on correlation analysis in karst drainage basin;
原理是利用相关分析间接实现差动电流虚拟三次谐波比较 。
The influence factors of low water based on correlation analysis in karst drainage basin;
原理是利用相关分析间接实现差动电流虚拟三次谐波比较 。
应用推荐