巖溶徑流 的英文怎麼說

中文拼音 [yánróngjìngliú]
巖溶徑流 英文
karst tun-off
  • 巖 : 名詞1. （巖石） rock 2. （巖峰） cliff; crag
  • 溶 : 動詞（溶化; 溶解） dissolve
  • 徑 : Ⅰ名詞1 （狹窄的道路; 小路） footpath; path; track 2 （達到目的的方法） way; means 3 （直徑的簡稱...
  • 流 : Ⅰ動1 （液體移動; 流動） flow 2 （移動不定） drift; move; wander 3 （流傳; 傳播） spread 4 （向壞...
  1. 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
  2. A study on the structure of karst aquifer medium and the groundwater flow in houzhai underground river basin

    后寨河流域巖溶含水介質結構與地下徑流研究
  3. 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。
  4. 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。
  5. 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 。
  6. This article will mainly introduce, analyze endangering characterstices of karst and the investigating methods in recharge area, runoff area, drainage area through engineering examples

    本文結合典型工程實例分別介紹了巖溶補給區，徑流區和排泄區的地質危害特點、類型及相應的勘察方法。
  7. 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。
  8. New achievements having been obtained in this field show that co2 participating in karst process in the epikarst dynamic system mainly comes from soil air co2 created by the organic carbon, in other words, although karst is a kind of biochemistric action in nature, distribution and transmit and cycle of carbon rely on changes of soil organic carbon. soil organic carbon is the greatest carbon storeroom. soil respiration emission of co2 is the most important passing entrance in carbon cycle of epikarst ecosystem

    已有的研究表明：參與巖溶作用的co _ 2多數屬于土壤中生物成因，也就是說，盡管巖溶作用是一種自然界無機化學作用，但碳的分佈與轉移及循環仍以生物活動為紐帶的土壤碳積累為轉化中心，土壤有機碳構成系統最大的碳庫，土壤呼吸碳表現為該系統中最重要的碳流通途徑，因此進行土壤co _ 2濃度觀測及其影響因子分析是研究表層帶巖溶生態系統運行機制和全球碳循環的首要條件。
  9. 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
  10. Based on the karst development pattern, groundwater enrichment pattern, and recharge, runoff and discharge conditions of groundwater, the karst areas distributed in the peripheral area of the basin is divided into 9 systems which are further divided into 25 subsystems

    在研究盆地周邊巖溶發育規律，地下水富集規律，地下水的補給、徑流、排泄條件的基礎上，將周邊巖溶區劃分為9個巖溶水系統，進一步劃分為25個巖溶水子系統。
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