巖溶地下水 的英文怎麼說

中文拼音 [yánróngdexiàshuǐ]
巖溶地下水 英文
karst groundwater
  • 巖 : 名詞1. （巖石） rock 2. （巖峰） cliff; crag
  • 溶 : 動詞（溶化; 溶解） dissolve
  • 下 : 下動詞1. （用在動詞后,表示由高處到低處） 2. （用在動詞后, 表示有空間, 能容納） 3. （用在動詞后, 表示動作的完成或結果）
  • 水 : 名詞1 （由兩個氫原子和一個氧原子結合而成的液體） water 2 （河流） river 3 （指江、河、湖、海、洋...
  1. Study on the seepage pollution of karst groundwater

    巖溶地下水滲漏污染研究
  2. Groundwater contamination by carbon tetrachloride in karstic area in china

    某市巖溶地下水四氯化碳污染特徵研究
  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. Generally, common geohydrology means only resolve partly the problems mentioned above, whereas, the isotope geohydrology plays an important role unrepiaced with other techniques in the research of karst groundwater

    通常，常規的水文地質方法解決上述問題的能力非常有限，而同位素水文地球化學在巖溶地下水的研究中所發揮的作用，是其它的技術方法難以替代的。
  5. 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
  6. 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
  7. Do springs and yellow river be the only sink of the karst - groundwater

    巖溶地下水主要的排泄點是否只有中、東部的泉和黃河
  8. Effects of forest community degradation on water chemical of karst shallow groundwater

    喀斯特森林群落退化對淺層巖溶地下水化學的影響
  9. Calculating supply amount of karst underground water in spring valley by synthetic permeance coefficieint method is introduced. the question of error in observing all area balanced calculation in fengfeng mine area is expouned

    應用綜合滲入系數法進行泉域巖溶地下水補給計算，解決了峰峰礦區用小流域觀測全區均衡計算過程中誤差較大的問題。
  10. 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。
  11. 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。
  12. Taian city belongs to north limestone area, and is a place taking karst ground water as source of water supply mainly

    摘要泰安地處北方石灰巖地區，是一個以巖溶地下水為主要供水水源的城市。
  13. The karst groundwater stores in the shallow karst zones below the surface, the middle karst zones controlled by geological structures and the deep zones of fossil karst

    巖溶地下水賦存於地表以下淺部巖溶帶、構造控制的中部巖溶帶和深部古溶蝕帶。
  14. Third, five schemes based on the combination different precipitation and pumping quantity is applied to the model prediction to predict the water laver in springs zone and high - point groundwater quantity exploited in 2010

    本通過對多種巖溶地下水開采方案預報對比，協調處理互為矛盾的「保泉」和「供水」目的，最終預報濟南市泉群地下水位標高，確定巖溶地下水的開采方案。
  15. The paper selects the subject entitled " the isoparametric finite - element three - dimension groundwater ( fe3dgw ) model for fracture - karst water resources and numerical simulation in jinan springs zone ", which is one sub - task of items on " exploitation and springs protection of jinan fracture - karst water ( no. 200001 ) " in this paper, the following questions are discussed : first, according to the site survey, and other relative datum, the condition of physical geography, geography and hydrogeology are summarized

    本文的研究課題? ?濟南市巖溶地下水數值模擬研究是山東省計委計劃項目「濟南市巖溶地下水開發利用與泉群保護研究（ no . 200001 ） 」的子課題。主要研究內容有：第一，在調查和閱讀分析相關資料的基礎上，概要總結和闡述泉群研究區域的自然地理、水文地質條件和地質概況，提出研究區水文地質概念模型，進一步建立濟南泉群研究區非均質各向異性三維非穩定流數學模型，利用等參有限元技術進行數值求解。
  16. Then the concept model of research zone and the isoparametric fe3dgw model for jinan springs zone is presented, and based on datum of 2001, 2002, we evaluate groundwater resources by means of numerical method. second, we apply the isoparametric fe3dgw model to evaluating groundwater resources in jinan springs zone, and present and optimize geography and hydrogeology parameters

    第二，將三維等參有限元技術運用至濟南巖溶地下水資源評價中，離散研究區域，優化滲透系數等水文地質參數，利用2001年和2002年的數據資料進行數值模擬和模型校正，採用多種巖溶地下水開采方案進行預報2010年的巖溶地下水動態。
  17. The deep karst groundwater has been clearly investigated on dynamics characters such as the retention time, the transportation speed, the flowing direction etc, and on the hydrodynamic connection with other groundwater aquifers

    調查了深部巖溶地下水的滯留時間、運動速度、徑流方向等動力學特徵，以及它們與其它地下含水層之間的水力聯系。
  18. Isotope evidence of strong runoff zones of karst groundwater in eastern weibei, shaanxi, china, and its renewability evaluation

    陜西渭北東部巖溶地下水強徑流帶的環境同位素證據及其可更新性評價
  19. As far as jinan fracture - karst water resources system concerned, keeping spring spurting and water supply are two major object functions, which are incompatible each other, while they are interdependent

    第三，對濟南市巖溶地下水系統來說，有「保泉」和「供水」兩個目標函數。
  20. The most important task object of all in the process of tunnel construction is karst groundwater. without investigating thoroughly basic condition and dealing appropriately with drainage problems, enormous economic loss would be occurred with hazards to tunnel construction

    巖溶地下水是隧道施工建設過程中最主要的工作對象，如果未能搞清楚巖溶地下水的基本情況，解決好排水問題，將會給施工帶來嚴重危害，造成重大的經濟損失。
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