karstic water 中文意思是什麼
karstic water
解釋
巖溶水-
The travertine has the character of surviving and perishing together with karstic water, lacking of saturated karstic water, the travertine landscapes would be blacken, spalled, sanded, and collapsed
鈣華具有「與水共存亡」之特性，失去飽和巖溶水滋養的鈣華會變黑、剝落、砂化、垮塌。 -
Based on the analysis of geothermal geology and hydrothermal convection system, the hot groundwater is formed from the mixing of the deep - circulating high - temperature structural - fissure water with the shallow circulating ordinary - temperature karstic water in the hydrothermal convection system
根據地熱地質條件及水熱對流系統分析，地下熱水是在水熱對流系統中由深循環高溫構造裂隙水與淺循環常溫巖溶水混合而成。 -
Water - bearing characteristics and hydro - geological models of karstic collapse columns in north china
北方巖溶陷落柱的充水特徵及水文地質模型 -
Abstract : according to observation and study, the paleokarstifications of ordovician could be classified into 6 periods, i. e. depositional karstification, weathering curst karstification, burial karstification, semi - burial structural karstification, second burial karstification stage, its karstic types have mainly deposition karst, emergence karst, burial karst, wqueezing - water and structural karst or hot - water karst, and its karst - rocks can be distributed to two kinds of types, i. e. karst - sedimentary rock and karst - regenerated rock, and further to 8 subcategories and 5 sub - sub - categories in the north of anhui, china
文摘:研究表明，皖北奧陶系古巖溶可劃分為沉積巖溶作用期、風化殼巖溶作用期、埋藏巖溶作用期、構造巖溶作用期和二次埋藏巖溶作用期；其巖溶類型主要有沉積巖溶、風化殼巖溶、埋藏巖溶或壓釋水巖溶和構造巖溶或熱水巖溶四種類型；其巖溶巖包括巖溶沉積巖和巖溶改造巖兩個大類，並可進一步劃分出8個亞類和5個子亞類。 -
According to observation and study, the paleokarstifications of ordovician could be classified into 6 periods, i. e. depositional karstification, weathering curst karstification, burial karstification, semi - burial structural karstification, second burial karstification stage, its karstic types have mainly deposition karst, emergence karst, burial karst, wqueezing - water and structural karst or hot - water karst, and its karst - rocks can be distributed to two kinds of types, i. e. karst - sedimentary rock and karst - regenerated rock, and further to 8 subcategories and 5 sub - sub - categories in the north of anhui, china
研究表明，皖北奧陶系古巖溶可劃分為沉積巖溶作用期、風化殼巖溶作用期、埋藏巖溶作用期、構造巖溶作用期和二次埋藏巖溶作用期；其巖溶類型主要有沉積巖溶、風化殼巖溶、埋藏巖溶或壓釋水巖溶和構造巖溶或熱水巖溶四種類型；其巖溶巖包括巖溶沉積巖和巖溶改造巖兩個大類，並可進一步劃分出8個亞類和5個子亞類。 -
After the saturated karstic spring was exposed to ground, for the changing of temperature, pressure, dynamics and the infecting of creatures, the ca / mgco3 deposited and turns into the travertine. the travertine heightened, and accumulated water to lakes, when the water brimmed over, waterfall came into being. this is the famous " stratified lakes and folded waterfalls " sight
該區鈣華系飽和巖溶水出露地表后，因溫度、壓力、水動力條件發生改變，加上生物作用的影響， ca / mgco _ 3析出堆積而成，並逐漸加高瀦水成湖；湖水充盈，疊水成瀑，從而形成了沿溝谷底層層疊疊分佈的「層湖疊瀑」奇景組合。 -
Maokou limestone karstic water flooding and harnessing in songzao coalmine, chongqing
重慶松藻煤礦茅口灰巖巖溶水害與治理 -
Analysis of the filling characteristics of karstic collapse pillars and its reactivation - induced water - conducting
巖溶陷落柱充填特徵及活化導水分析 -
Hydrogeological and mechanical basics of water inrush from karstic collapse columns in northern china
華北巖溶陷落柱突水的水文地質及力學基礎
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