巖溶動態 的英文怎麼說

中文拼音 [yánróngdòngtài]
巖溶動態 英文
karst regime
  • : 名詞1. (巖石) rock 2. (巖峰) cliff; crag
  • : 動詞(溶化; 溶解) dissolve
  • : 名詞1. (形狀; 狀態) form; condition; appearance 2. [物理學] (物質結構的狀態或階段) state 3. [語言學] (一種語法范疇) voice
  1. 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水分佈特點、水的成因及形成的環境背景,確定地下水的補給源區、補給高度、位置及區內大氣降水,地表水、地下水的循環關系,劃分出水不同的水文地質單元; 2
  2. So it is chiefly that soil co2 concentration and its influencing factors should be studied in ordered to learn the mechanism of epikarst ecosystem and global carbon cycle. karst dynamics laboratory, ministry of land and resources, has been studied the mechanism of seven typical epikarst ecosystem and global changes through igcp 299 ( geology, climate, hydrology and karst formation, 1990 - 1994 ) and igcp 379 ( karst processes and the carbon cycle, 1995 - 1999 ) to igcp 448 ( world correlation of karst ecosystem, 2000 - 2004 ), while observation and analysis and research of epikarst ecosystem in mt. jinfo have just been beginning. the thesis analyzes that based - on observational point of green pond and deep dell in the west slope of jinfo mountain, co2 concentration and regularity of epikarst ecosystem contrasting woodland with uncovered land have been studied through the observation of temperature and humidity and co2 concentration

    國土資源部力學開放研究實驗室以igcp229 、 igcp379和igcp448項目為依託,開展了我國7個典型的表層帶系統運行規律及其全球變化影響研究,而其中金佛山的觀測、分析與研究則才剛剛起步,本文以金佛山西坡摘公碧潭幽谷為觀測點,主要通過coz濃度、溫度和濕度的觀測,開展林地表層帶系統與裸地表層帶系統coz濃度特徵及其變化規律的對比研究,這對進一步深入研究系統運行機制和全球碳循環以及開展全球對比有著重要意義。
  3. As a hard - core part of epikarst ecosystem, soil makes a hinge action in the karst process. it forms a leach layer between rainfalls and carbonate and gives a great much time and space in the karst process. soil co2, a very pivotal factor in the karst dynamic factors, makes an action of driving forces in karst dynamic system

    土壤作為表層帶系統的核心部分,在過程中起著樞紐作用,它的存在使得大氣降水與碳酸鹽之間形成一個「過濾層」 ,賦予作用更廣闊的時間和空間,其中土壤co _ 2是個非常關鍵的因子,它是作用的重要物質來源,在力系統中起著驅力作用。
  4. The research include : 1 ) measuring co2 concentration in the soil air and vegetation air by using co2 measuring instruments ; 2 ) measuring the releasing rate of co2 coming from soil surface by using alkaline absorbing method ; 3 ) measuring the hydrochemical indexes of soil water. the research results are as follows : ( 1 ) the author has made field observation of depth distribution of soil air co2 in the mt. jinfo karst experiment site. the results show that two concentration gradient, soil to atmosphere and soil to carbonate rock, are form

    本次實驗以典型的亞熱帶分佈區?金佛山自然保護區為例,選擇了窪地內的高山草甸和靠窪地邊緣地帶的方竹林、裸地以及石林內的喬木林4個樣地,對土壤co _ 2濃度空間分佈規律以及晝夜和日變化狀況進行了觀測,獲得了如下新的認識: ( 1 )土壤中co _ 2濃度分佈的觀測結果表明,土壤中具有土壤-大氣、土壤-碳酸鹽兩個方向的co _ 2濃度梯度。
  5. First, on the base of investigating geleshan geologic environments, the author carefully analyzes them, studies their water storage structure, discusses the relationship of underground water dynamic changes and tunnel drainage by desiccation ; secondly, the author makes the dynamic analysis, regression analysis, routine hydrochemistry analysis, isotope analysis, so draws to guan - yin gorge anticlire east and west slot ' s karst developing features, alternated conditions underground water and supplying drain ways ; thirdly, by stating the fissuring ' s surveying data, the author calculates the seeping tensor

    作者在進行歌樂山地質環境調查的基礎上,仔細分析了大量觀測資料,研究其儲水構造,掌握地下水變化與隧道施工涌水的關系,及補給受降雨的影響情況。對隧道周圍的地下水進行分析、回歸分析、常規水化學分析以及同位素分析,得出觀音峽背斜東西翼槽谷的發育特徵,及地下水的循環交替條件、補給排泄途徑;統計分析裂隙測量數據,計算滲透張量。
  6. So karst vegetation is charactered by petrophile, xerophile and calciphihe in those areas where soil cover is very thin, and the underground drainage system is well developed. the running of karst ecosystem is controlled by two subsystems, which are karst dynamic system in inorganic life and genetic information transmitting system in organic life

    系統的運行受到兩個子系統的聯合作用驅,即無機方面的「力系統」和生命方面的「遺傳信息傳遞系統」 ,但主要受以碳、水、鈣循環為中心的力系統的控制。
  7. 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,採用多種地下水開采方案進行預報2010年的地下水
  8. 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的分析,確定了泉水流量的影響因素,建立了泉水流量的衰減方程和泉水流量的預測模型,預測了天然狀泉水流量,評價了泉域水的開采資源。
  9. The ordovician carbonate reservoir in tahe oilfield is characterized by deep buried depth, multiple storage spaces, complex reservoir type, which lead to difficult reservoir simulation and performance prediction for the existing simulators are hard to simulate the dual porosity reservoirs

    摘要塔河油田奧陶系碳酸鹽油藏埋藏深,儲集空間多樣,儲集類型復雜,油藏模擬和預測難度大,其原因主要是現有的油藏數值模擬器很難模擬裂縫洞型雙重介質系統。
  10. Through the research of paleo - environment change and process with regard to east asia monsoon environment system, loess, karst, ice core, lakes, paleo - oceanography, the impact of human activities over terrestrial ecological system, and marine ecologic dynamics, they rebuild the natural environment evolution regularity of east asia, thus actively and effectively push forward the research of global change study

    通過東亞季風環境系統、黃土、、冰芯、湖泊、古海洋學和人類活對陸地生系統影響以及海洋生力學等方面,開展古環境變化和過程研究,重建了東亞自然環境演化規律,積極而卓有成效地推了全球變化研究。
  11. 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:參與作用的co _ 2多數屬于土壤中生物成因,也就是說,盡管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系統運行機制和全球碳循環的首要條件。
  12. This paper sums up present and history karst collapse in tai ’ an, shandong province. it mainly spreads in the quaternary system cover areas where the looser layers are thinner, underlying open karst caves and cracks are under the quaternary system

    本文分析了山東省泰安市地面塌陷的形成歷史及現狀,從地下水及地質環境監測結果入手,研究得出塌陷主要分佈在鬆散層較薄的第四系覆蓋區,發生時間主要集中於枯水年份或年內枯水期和豐水期初。
  13. Dynamic balance process and instability process of rock - salt cavity roof are studied, and instability mechanism of rock - salt cavity roof is studied with catastrophe theory, and the influencing factor are analyzed, which will be theoretical basis of rock - salt cavity stability control

    為此,分析了腔頂板平衡過程及失穩發展機制,並利用突變理論研究了腔頂板失穩機理,探討了腔頂板穩定性的影響因素,從而為腔穩定性拉制打下一定的理論基礎。
  14. The paper sets up a groundwater three - dimensional flow model to predict the karst groundwater regime in east area of wei bei in shanxi province on the condition of exploitation

    本文建立地下水三維流模型,對陜西省渭北東部的地下水開采條件下的進行預測。
  15. According to karstic groundwater supply and demand status in the region, especially through numerical simulation of current karstic groundwater, the author considered that there still has proper development potential of karstic groundwater in western handan

    摘要根據區域內地下水供需現狀,特別是通過對地下水最新開采的數值模擬,認為邯鄲市西部水區具有一定的開發潛力。
  16. The research results are as follows : ( 1 ) with the increasing of the height to the ground, the value of co2 concentration in air become adding ; the depth of soil profile more deeper, the value of co2 concentration in soil more higher. ( 2 ) the temperature in the sample area, which is with high elevation, is higher than the temperature in the sample area, which is with low elevation

    通過研究發現: ( 1 )兩不同海拔高度上的樣地內大氣co _ 2濃度值均具有隨距地表高夏季金佛山垂直自然帶匕系統內co :的研究度的增加而減少的趨勢;而土壤空氣中的c0 :濃度值多具有隨土深增加而增大的趨勢。
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