karst geology 中文意思是什麼

karst geology 解釋
巖溶地質學
  • 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]。
  • geology : n. 1. 地質學。2. (某一地區的)地質。3. 地質學的著作。
  1. Qingjiang bridge karst geology drill hole pile construction

    清江大橋巖溶地質鉆孔樁施工
  2. By the check - out, inspection and measurement to start construction the industrial art to this test pile with the examination between stake body mass and bearing power, made sure the stroke reasonable operation method drilling under the dissolved cavern geology term ; the pier foundation loading test expressed the lading and rub the lading that resistance drag a glazing for of relation, and to the borehole cast - in - place concrete pile in the karst terrain deliver with break the mechanism, the characteristic of bearing power, proceeding the spot test job of the full of result ; the test data expresses the stake side friction resistance to rises with a bat batch terminal friction resistance very important function, the of tip of pile resistance drag occupies the proportion very few

    通過對本次試樁施工工藝的檢測和樁身質量及承載力的檢驗,確定了沖擊鉆在溶洞地質條件下的合理使用方法;基樁承載實驗表明了荷載與摩擦阻力之間的關系,並對巖溶地區的嵌巖灌注樁的荷載傳遞和破壞機理、承載力特性,進行了富有成果的現場測試工作;試驗數據表明樁側摩阻和支盤端阻起很重要的作用,樁端阻力所佔比例甚少。這與設計樁基時的計算模式相差很大,承載力也較設計增加;使用力學數值分析方法和有限單元法,對鉆孔灌注樁樁端下的巖體強度和結構穩定性方面進行模擬計算和定量研究。
  3. The species richness and diversity index order of coniferous and broad - leaf forest and evergreen broad - leaf forest in different geology plots was as follows : shrub layer > herb layer > tree layer ; in shrub plots, the order was herb layer > shrub layer. in general jsw, jsi and ea index order was herb layer > shrub layer > ree layer. that indicated that the species of tree and shrub in karst area distributing is not even, and the species, which are dominant and adapt to the karst environment are cleaer

    不同地區樣地針闊混交林和常綠闊葉林物種豐富度指數、多樣性指數均表現為灌木層草本層喬木層,而在灌叢樣地,物種豐富度和多樣性指數表現為草本層灌木層;整體上,石灰巖地區樣地jsw 、 jsi和ea指數為草本層灌木層喬木層;砂頁巖地區樣地為灌木層草本層喬木層。
  4. 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

    國土資源部巖溶動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個典型的表層帶巖溶生態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,開展林地表層帶巖溶生態系統與裸地表層帶巖溶生態系統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巖溶生態系統運行機制和全球碳循環以及開展全球巖溶生態對比有著重要意義。
  5. This paper adopts the land use state in2000a ( l : 3 + 104 ), the soil chart ( 1 : 6 + 104 ) and hectometer contour relief map ( include three chongqing area ) of chongqing and geology map ( l : 6 + 104 ) of sichuan province as basic analytical data, measure landscape patches into 7 types including cultivated land, orchard, forestland, unused land, grassland, resident and industry land, water bodies according to land use state basing on land use types, make the landscape map of chongqing karst area by gis software

    本研究是以重慶市1 : 30萬的土地利用現狀圖( 2000年版) 、 1 : 60萬的土壤圖以及重慶市百米等高距的地形圖和四川省(包括重慶市) 1 : 60萬的地質圖作為基本分析圖件。在土地利用類型的基礎上,依據土地利用現狀劃分了耕地、園地、林地、未利用地、草地、居民工礦用地和水域7類景觀嵌塊體類型,再藉助于gis軟體生成重慶巖溶區景觀圖。
  6. The status of investigation to karst in yanping freeway are discussed, and engineering geology characteristic and problem of karst are analyzed, and then engineering geology sorting and treatment principle are put forward to karst in yanping freeway ; so this paper has a certain extent refence and instructional function for the construction of highway in karst region

    摘要文章敘述了硯平高速公路巖溶勘察情況,分析了硯平高速公路巖溶的工程地質特徵及工程地質問題,提出了硯平高速公路巖溶的工程地質分類及處治原則,對巖溶地區公路的建設具有一定的參考和指導作用。
  7. It is generally accepted that karst ecosystem controlled by geology is fragile. this is the result of soluble rock dissolution, which brings about shortage in soil and water on the surface

    巖溶生態系統是受巖溶環境制約的生態系統,以石生、早生及喜鈣和地下空間為特徵,一種由地質條件所決定的脆弱環境。
  8. Karst water was divided to several area and was protected with respectively protective measures according to the comprehensive analyse about geology, hydrogeology and pollution situotion

    根據其富水規律、目前巖溶水遭受污染的情況以及地質、水文地質的綜合分析,對巖溶水進行了保護分區,並提出各級保護措施。
  9. 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。
  10. On the basis of previous research view to the boundary of karst - groundwater system in research area, chapter two starts with the natural geography condition of research area and analyzes the condition of geology and hydrogeology carefully. accordingly, several queries are brought out as follow : is the tertiary system ( n ) confining layer

    第二章從研究區自然地理條件入手,結合前人研究區巖溶水系統邊界的研究觀點,對研究區的地質、水文地質條件進行了深入分析之後,提出如下問題:第三系( n )地層是否為隔水
  11. The origin and development of stone forest has attracted many karst researchers home and abroad, and they have done some macroscopical and microscopical studies on stone forest in terms of such conditions for its development as geology, climate, hydrological process, sub - soil corrosion, geomorphological types, history of development, paleo - geographical enviroment and biological effects etc, and put forward some development models, however, most of the studies just pay their attention to some single aspects of the problem

    石林的成因及發育演化問題引起了國內外喀斯特學者的關注,他們從地質、氣候、構造、水文過程、土下溶蝕過程、地貌成因類型、發育年代、發育歷史和古地理環境以及微形態的生物作用過程等方面對石林的形成發育進行了宏觀和微觀的研究,並提出了相應的發育演化模式,但多側重於單一方面的研究。
  12. Constructive method of pile foundation under karst double layer geology and common situations handling

    巖溶夾層地質樁基施工方法及常見情況處理
  13. Karst geology terminology

    巖溶地質術語
  14. Academia summary on the western conference of hydro - power development and karst hydro - engineering geology

    西部水利水電開發與巖溶水文工程地質學術研討會學術總結報告
  15. So it is difficult to forecast the karst collapse ’ s time and place. on the other hand, we can evaluate the possibility of karst collapse by surveying the enigeering geology particularly. in other words, prevention and drawing building ’ s layout decide by the stability of karst collapse

    但是,根據當地的巖溶發育程度,則可以通過詳細的工程地質調查,來評價巖溶塌陷發生的可能性大小,即巖溶塌陷的穩定性,尋找潛伏的巖溶洞穴,作為防治塌陷及制訂工程建設規劃的依據。
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