karst water 中文意思是什麼

karst water 解釋
喀斯特水
  • karst : n. 【地質學；地理學】水蝕石灰巖地區；巖溶。 karst cave 水蝕石灰洞[喀斯特]。
  • water : n 1 水；雨水；露；〈常作 pl 〉 礦泉，溫泉；藥水。2 〈常 pl 〉水體；水域；水道；海；湖；河；海域；...
  1. Harness technology for karst water in ordovician limestone with underground grouting of hole

    井下鉆孔注漿治理奧灰水技術
  2. Isotopic tracing analysis of round - axis flow of karst water in maoba syncline

    毛壩向斜核部巖溶水繞軸徑流的同位素示蹤分析
  3. Analyses of karst water circulation system in xuzhou hydrogeological unit

    徐州市水文地質單元巖溶地下水循環系統分析
  4. Through calculating the age of shallow and deep groundwater, the velocity of karst water cycle has been obtained

    分別計算了淺層和深層地下水的年齡，確定了巖溶水的循環速率。
  5. On this basis, it also studies the main recharge of groundwater, discusses the relationships between river and groundwater, shallow confined water and phreatic water, northern karst water and quaternary phreatic water as well, and get the recharge percentage which river recharges to phreatic water

    在此基礎上，研究了地下水的補給來源，探討了河水與地下水、淺層承壓水與潛水、北部巖溶水與山前第四紀潛水之間的相互關系，確定了河水對潛水的補給比例。
  6. On the regional karst water, it has been primarily clarified that the distributing trait, the cause of formation, and the environment background, and it has been confirmed that the source, the height, and the location about the karst groundwater replenishment. we have found out the relationship of developing circulation among the atmospheric water, the surface water, and the groundwater in the research area, and have compartmentalized the different geohydrology structures about the karst water. 2

    初步查明了研究區的巖溶水分佈特點、巖溶水的成因及形成的環境背景，確定巖溶地下水的補給源區、補給高度、位置及巖溶區內大氣降水，地表水、地下水的動態循環關系，劃分出巖溶水不同的水文地質單元； 2
  7. Study on environmental isotopic features of the karst water and the yellow river water around the juncture of shanxi, shaanxi provinces and inner mongolia autonomous region

    晉陜蒙接壤地區巖溶地下水與黃河水環境同位素特徵分析
  8. The chemical action of karst water compositions of the ordovician in luan mining area

    潞安礦區奧陶系巖溶水化學成分的成因
  9. Combing the linear seepage model with hydrogeology in the region of zhong - liang reservior, the analysis of the problem of positive and negative is emphasized. make use of with some observing information of boreholes in this region, adverse seeking the hydrogeology of the reservoir in the region with finite element method, the leakage quatity of karst water in the region of reservoir is forecasted.

    線性滲流模型結合了中梁水庫庫區水文地質條件，重點進行正反問題的計算分析，利用研究區若干觀測孔資料，採用有限單元法反演庫區的水文地質參數，並預測了庫區巖溶水滲漏量。
  10. According to theory of the environmental isotope tracer and theory of deuterium excess ( d - excess ) parameter with the atmospheric water and the groundwater, the dissertation has comprehensively researched on the regional karst water and the pressure - bearing karst water in deep maoba syncline in virtue of routine geologic and geochemistry investigation

    根據環境同位素示蹤、大氣降水氘過量參數和地下水氘過量參數演化理論，結合常規地質、地球化學工作，對該地區域巖溶水和毛壩向斜段核部深層巖溶承壓水進行了綜合分析研究。
  11. The farther knowledge has been acquired that pressure - bearing karst water in deep maoba syncline is replenished by the atmospheric water from both east wing and west wing of maoba syncline, but which from east wing is more, and it is impossible that the pressure - bearing karst water from west wing rounds to replenish east wing. 3

    得到進一步的認識；毛壩向斜核部的深部承壓水，同時接受向斜東翼和西翼大氣降水的補給，東翼的補給量相對大些；整個深部承壓水不存在西翼繞過核部補給東翼的可能性； 3
  12. On the basis of anatomizing the condition of hydrogeology with zhongliang water resources and power engineering, combined with the data analysis of flux with surface water, aquatic chemistry, and experiment of tracing, the condition of karst leakage in the region of reservoir is educed. the concept of reservoir leakage with these information is put forward, the leakage quantity of karst water in the region of reservoir with the method of water equilibrium is applied

    在仔細分析中梁水利水電工程庫區水文地質條件的基礎上，結合地表水測流資料、水化學分析資料及示蹤連通試驗資料，得出水庫區巖溶滲漏條件，並在此基礎上提出水庫滲漏概念模型，採用水均衡法計算出庫區的巖溶水滲漏量。
  13. Karst water gushing and mud soil projecting hazards and their harnessing schemes ' selection in the east flank of tongmaling anticline in yuanliangshan tunnel of yuhuai railway

    渝懷鐵路圓梁山隧道桐麻嶺背斜東翼巖溶涌水突泥災害與整治方案比選
  14. 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

    在上述三種計算庫區巖溶水滲漏量的模型中，由於線性?非線性滲流模型同時考慮了與中梁水庫區實際情況相符合的達西流和非達西流區域並存的地下水運動，因此，利用該模型計算出的庫區巖溶水滲漏量更合理。
  15. Karst water was divided to several area and was protected with respectively protective measures according to the comprehensive analyse about geology, hydrogeology and pollution situotion

    根據其富水規律、目前巖溶水遭受污染的情況以及地質、水文地質的綜合分析，對巖溶水進行了保護分區，並提出各級保護措施。
  16. Considering the seepage of linear and the seepage of non - linear in the karst area are always coexisting, the model of linear seepage and non - linear seepage is put forward firstly on the basis of domain decomposition method. the movement of groundwater in an ideal model is simulated with this method, and the program of dar - nondar. for is compiled. then these results are applied to zhongliang water resources and power engineering, the leakage quantity of karst water is calculated

    考慮到巖溶區滲流往往都是線性流與非線性流並存，首次提出了基於區域分解法理論的線性?非線性滲流模型，利用該方法模擬出理想模型中的水流運動，並編制了計算程序dar - nondar . for ，然後將該成果應用於中梁水利水電工程中，預測出庫區巖溶水滲漏量。
  17. This article introduced the method of geological investigation of nanling tunnel karst disease, elaborated the tunnel engineering geology conditions, especially the karst water, the karst water power channel and the harm of karst water, and analyzed the cause that produced the karst disease

    摘要南嶺隧道巖溶地下水活動造成地表坍陷、洞內泥砂淤塞等病害，其原因在於隧道施工遺留的導洞長期疏排巖溶水，採用地質測繪、物探、鉆探、水文地質試驗等綜合勘察方法，查明地下水通道位置、地下水流速、流向，針對病害原因，提出攔截、封團、疏排、填充等綜合整治方案。
  18. Drinking groundwater source in the city of xingtai lies in baiquan karst water system of runoff and emission which is in front of the taihang mountains

    摘要邢臺市區地下飲用水源位於太行山前儲存兩種相當豐富的巖溶水和孔隙水的百泉泉域徑流排泄區。
  19. The karst water moves from south to north. after moving to jinan city, the karst water is blocked by igneous bodies, the karst water passes through fissures and karst and gushes out to the surface as springs

    來自南部補給區的巖溶地下水徑流至老城區附近，遇到巖漿巖體阻隔，在地形低洼部位通過淺部石灰巖巖溶裂隙湧出地表，形成濟南諸泉。
  20. Based on the analysis of hydrogeological conditions in the study area, calculation and chose of the hydrogeological parameters was performed by ga, and three methods were used to evaluate groundwater resources of yangzhuang karst water system in this paper. calculation and analysis of water resources carrying capacity of yangzhuang basin were set up. as well as suggestions of protection about yangzhuang karst water system was provided clearly

    在分析研究羊莊盆地水文地質條件的基礎上，應用遺傳演算法（ ga ）進行水文地質參數優選，並利用三種方法計算評價了羊莊巖溶水系統的可采資源量，計算分析了羊莊盆地的水資源承載能力，並提出了增源增采及分級保護的措施。
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