巖溶泉 的英文怎麼說

中文拼音 [yánróngquán]
巖溶泉 英文
karst source
  • 巖 : 名詞1. （巖石） rock 2. （巖峰） cliff; crag
  • 溶 : 動詞（溶化; 溶解） dissolve
  • 泉 : 名詞1 （泉水） spring 2 （泉眼）the mouth of a spring; spring3 （錢幣的古稱） an ancient term for...
  1. Water invasion bursten out during the railway - tunnel construction is usually the mainly problem in constructing or operating, also which brings surface water to exhaustion and pollutes environment or effects ecology, etc. the geleshan tunnel which crosses through guan - yin gorge anticline which trend is near south north, is located between tuanjie village and jingkou village of the shapingba zone, chongqing city, which is belongs to the inducting segment of yu - huai railway. the guan - yin gorge anticline appears to ridge and slot interlacing in land form, and is composed of clastic rock and carbonate rock from jurassic xintiangou group to triassic

    歌樂山隧道位於渝懷線引入段重慶市沙坪壩區團結村至井口村之間，隧道穿越近南北向的觀音峽背斜，地貌上表現為脊、槽相間，觀音峽背斜由侏羅系新田溝組至三疊系下統碎屑巖和碳酸鹽巖組成，歌樂山頂大部分出露可溶巖地層，地表巖溶發育，有大量泉水和暗河出口，並修建有多個中小型水庫、大量池塘和水井。
  2. Physical - chemical characteristics of jinfushan karst spring in chongqing

    重慶金佛山碧潭泉巖溶泉水的物理化學特徵
  3. With practical engineering examples, this paper describes the application of gpr to engineering investigation of such harmful geological structures as karst, faults and fractures

    摘要結合貴州福泉下翁溪水庫、芙蓉江沙阡電站、冗各電站3個工程實例，介紹探地雷達勘探在巖溶、斷層破碎帶等不良地質構造勘察方面的應用。
  4. 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
  5. 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。
  6. 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。
  7. 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。
  8. Infiltration of atmosphetic water and river leakage are the major supply source of krast water in jinan spring field, while artificial water - taking and spring discharge are its major discharge forms. the karst water flows from south to north in the whole and the average recharge capacity is 55 x 104m3 / d

    巖溶水補給來源主要為大氣降水滲入和河流滲漏，排泄方式主要為人工開采和泉水排泄，總體向北徑流，泉域多年平均補給量為55萬m ~ 3 d 。
  9. 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。
  10. 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。
  11. Based on successive regression study of observation data, the authors ascertained the factors having influence on the fluctuation in the bai spring discharge, established the regression equation and the prediction model, and calculated the exploitable karst water resources under natural conditions

    摘要本文通過對輝縣自泉泉水流量動態的分析，確定了泉水流量動態的影響因素，建立了泉水流量的衰減方程和泉水流量的預測模型，預測了天然狀態泉水流量，評價了泉域巖溶水的開采資源。
  12. The jinan spring catchment is a complicated karst water system, the following major work had been done in order to discuss the proplem of spring protection and water supply. 1. having conduced exploration, experiment and comprehensive research, the southern boundary of the jinan spring catchment is determined to be the surface water divide ( changecheng mountain ), the source of yufu river and baedasha river ; the northern one is the carbonniferous and permian strata, together with the igneous rock mass in the north of jinan, and the eastern and the western ones are dongwu and mashan faults respectively, which are weakly permeable boundaries. the total area of the spring catchment is 1486 km2

    濟南泉域為一復雜的巖溶水系統，為了探討保泉供水問題，主要做了以下工作： （一）經過勘查、試驗和綜合研究確定濟南泉域邊界是：南邊界為玉符河、北大沙河源頭的地表水分水嶺（即長城嶺） ；北邊界為濟南北部的石炭、二迭系煤系地層和巖漿巖體；東、西兩側分別以弱透水的濟南東部的東塢斷裂和西部的馬山斷裂為邊界。
  13. 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。
  14. However, with the advancement of society and economy, unblanced water input and output, the water consumption in the city increases so rapidly that karst groundwater, the source of the jinan springs, has been over extracted heavily

    但近幾年來，隨著社會經濟的發展和人口的增加，水資源量收支失衡，濟南泉水之源? ?巖溶地下水被超量開采。 90年代，僅濟南市區、東郊、西郊水源地的集中開采量就達到55 60萬立方米日。
分享友人
分享到 Line

分享到臉書