karst spring 中文意思是什麼

karst spring 解釋
喀斯特泉
  • 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]。
  • spring : n 1 春季,春天。2 青春;初期。3 〈pl 〉大潮時期。4 泉。5 源頭,水源,根源,本源;發生;動機,原動...
  1. 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
  2. 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。
  3. 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 。
  4. 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。
  5. 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。
  6. 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。
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