Chinese translation for "地下水运动"

ground water movement
groundwater movement
subsoil water movement
travel of underground water

Related Translations:

地下水调节:  groundwater conditioninggroundwater regulation

地下水化学:  groundwater chemistry

地下水截流:  groundwater trapping

地下水怜:  underground water flow

地下水缸:  sumcistern

地下水质量:  groundwater quality

地下水方程:  ground water equationgroundwater equation

地下水压力:  artesian pressureground water pressuregroundwater pressure

地下水屏障:  groundwater barrierhydrologic barrier

季节性地下水:  temporary water

Example Sentences:

	1.	Surface erosion , surface infiltration and movement of ground water are possible triggering mechanisms of failures in loose filled slopes 地表水冲蚀与渗入、地下水运动都可能引发松散斜坡破坏。
	2.	Finally , this question for study is put forward . the basic equations of underground water movement and groundwater contamination are drawn in chapter 2 论文第二章先对封闭圩区共性进行概化，然后针对封闭圩区，推导出了其地下水运动方程和溶质迁移方程。
	3.	It result in water level rising , hypo - salinification aggravating , sediment silting up , the lake atrophy , marsh extending and nature disaster such as droughu waterlog ^ salinification occurring frequently . completely analysis to geology and hydrology conditions of the district along yellow river in shandong has been applied in this paper and aquifer ' s hydrological characteristic and subsurface flow ' s characteristic have been analysed as keystone in the paper . after finding out the distribution rule and formation conditions of the shallow layer " s ground water resource , divide the district into three hydrological sections according to hydrological conditions and subsurface flow characteristic 本文对山东沿黄地带地质、水文地质条件进行了全面系统的分析，并重点分析了区内含水层的水文地质特征及地下水运动特征，进一步查明了浅层地下水资源的形成条件和分布规律，根据水文地质条件及地下水运动特征，划分出三个水文地质区，划分并论证了粘土裂隙含水层的形成及供水意义；确定了科学的水文、水文地质参数，为准确地计算浅层地下水资源奠定了可靠的基础；根据浅层地下水资源形成特点，建立了地下水均衡方程式，据此，计算了区内浅层地下水资源及浅层地下水可采资源。
	4.	In view of geological and hydro - geological situations of the south anchor runyang yangtze river highway bridge , the paper bring forward mathematical model and calculation method of double deck structure groundwater , which can be used to lively calculate every layer ' s water table , so that we can realize every layer ' s settlement calculation and control ; establish the inter relationship between non - linear physical - mechanics parameter and hydro - geological parameter , objectively describe the non - linear change process of the porosity , hydraulic conductivity , specific storativity in the process of soil dewater and concretion 针对润扬长江公路大桥南锚场地地质、水文地质条件提出了双层结构地下水运动的数学模型和计算方法，该方法可以实时计算出各分层的地下水位，实现了各分层沉降计算与控制研究；建立了土层非线性物理力学参数与水文地质参数之间的内在联系，客观地描述土层降水? ?固结过程中孔隙度、渗透系数和贮水率等参数非线性变化过程。
	5.	On the foundation of reference researches , through analyzing the condition of rainfall and hydrogeology of tian - tang river in the suburb of south - east of beijing , the mathematical models of the shallow ground water movement were founded . according to the experiment result of pump water and other reference data , the parameter of hydrogeology and ground water were established . on the foundation of present and future trend of using water on industry , agriculture and living , the solution of mathematical models were calculated by the method of finite element 在前人研究的基础上，本文通过对北京市东南郊天堂河流域降雨、水文地质条件的分析，建立浅层地下水运动数学模型，根据抽水试验结果并参考有关资料确定水文地质和地下水补给的有关参数，根据工业、农业、生活现状用水情况及未来的发展趋势，采用有限元的方法对地下水运动数学模型进行求解。
	6.	It is usually difficult to confirm the boundary condition in dewatering engineering of deep foundation pit . and the variety of the exploring results often make engineers difficult to accurately get hold of the hydraulic geological parameter . it could n ' t accurately set up the model of underground water movement 在深基坑降水工程中，边界条件通常难以确定，工程勘测结果的多样性常常使工程技术人员难以准确把握水文地质参数，使用确定的地下水动力学原理也不能准确建立地下水运动模型。
	7.	The paper solved unsteady groundwater flow equation with the mentioned disperse pattern and the results have shown its stabilize astringency . the method was applied to manipulate groundwater in shuishy area , dalian and got satisfied results . this method can also be applied in other relevant fields 本文用它求解非稳定流地下水运动方程，并证明了算法稳定性及收敛性；还用这种方法对大连水师营地区地下水运动状况进行了数值模拟，且取得了较好的效果，此法也可在其它类似计算中推应用。
	8.	Finally , some questions that are relative with isoparametric fe3dgw model , such as prediction for rainfall are presented and applied to evaluation for jinan fracture - karst water resources . from the concept of system , the ultimate metabolic equation of groundwater for protecting water resource is discussed here 第四，探讨与地下水运动数学模型的相关问题，包括数学模型输入项大气降水量的预报，地下水代谢方程的研究，将传统的时间序列方法加以改进，并应用于地下水资源评价。
	9.	In the three models of calculating the leakage quantity of karst water , on account of the linear and non - linear seepage model are accord with the movement of darcy flow and non - darcy flow coexists with the practical instances in zhong - liang reseviour , so the calculation result of leakage quantity of karst groundwater with this model is more reasonable 在上述三种计算库区岩溶水渗漏量的模型中，由于线性?非线性渗流模型同时考虑了与中梁水库区实际情况相符合的达西流和非达西流区域并存的地下水运动，因此，利用该模型计算出的库区岩溶水渗漏量更合理。
	10.	On basis of the history of research on the development of groundwater modeling in the area of karst , this paper presents the summary of basic theory of karst water movement . the main concerned methods used to model the movement of karst groundwater are summarized systematically and comprehensively . the advantages and disadvantages of every calculation methods are analyzed and compared , based on the analysis , the adaptability of these methods are clarified 回顾了岩溶区地下水流运动数值模拟的发展历程，概述了岩溶水运动的基本理论，系统全面地总结了国内外有关岩溶区地下水运动数值模拟方法，分析比较了各种计算方法的优缺点，在此基础上给出了各种计算方法的适用条件。

Similar Words：

"地下水源" Chinese translation, "地下水源地" Chinese translation, "地下水源枯竭" Chinese translation, "地下水越流" Chinese translation, "地下水允许开采量" Chinese translation, "地下水运动（渗流）" Chinese translation, "地下水蕴藏量" Chinese translation, "地下水灾" Chinese translation, "地下水再补给" Chinese translation, "地下水增补" Chinese translation