basin karst 中文意思是什麼
basin karst
解釋
盆地喀斯特-
Vulnerability of karst aquifers in houzhai river basin and its relations with landuse change
后寨河流域巖溶含水層脆弱性及其對土地利用方式的響應 -
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 -
This article is based on statistic and analysis of the long - term observation data of the groundwater in the karst basin from 1987 to 2005 and systematically discusses the water level of karst groundwater, the pumping volume and the carved distribution regulation because of over - pumping water and puts forward some specific measures to reasonably development and utilization of groundwater resources
摘要通過覆蓋型盆地巖溶盆地中取水深井1987年2005年盆地地下水長觀資料統計分析，系統探討了宕溶地下水的水位、取水量以及抽水產生的塌陷分佈規律，提出了合理開發利用地下水資源的具體措施。 -
It has been used in many fields such as machinery industry, electronic industry, power industry, hydraulic engineering, chemical industry, agriculture, environment, economy and so on. this paper focuses on application of anns in the study of the karst basin and its low flow
人工神經網路是一門正在迅速發展的交叉科學，現已廣泛應用於機械工業、電子工業、能源工業、水利工程、化學工業、農業、環境和經濟學等學科。本文主要討論人工神經網路在喀斯特流域及其枯水徑流研究中的應用。 -
The main conclusions are as follows : the hco3 - ion content of zhujiang river changes notably in one hydrological year, especially in wet season and dry season. as for the content of inorganic carbon, that of the xijiang river is the highest, then the beijiang river, and then the dongjiang river. the xijiang river ' s inorganic carbon source was major from karst process in the drainage basin
得出如下的結論：珠江水體hco _ 3 ~ -離子含量在一個水文年中發生顯著變化，特別是豐水期與枯水期之間波動幅度較大；無機碳含量西江含量最高，其次是北江，東江最低；西江無機碳主要來源於巖溶作用，由於受河流沖刷效應影響，豐水期hco _ 3 ~ -離子含量升高；東江流域無機碳主要來源於硅酸鹽巖的碳酸鹽風化過程，豐水期hco _ 3 ~ -離子含量無顯著變化；北江無機碳來源於巖溶作用和硅酸鹽巖的碳酸鹽風化過程，受稀釋效應影響，無機碳含量隨水量增加而降低。 -
Society economy evaluation of typical karst cell in lijiang river basin
灕江流域典型巖溶單元社會經濟狀況評價 -
Based on the analysis of hydrogeological conditions in the study area, calculation and chose of the hydrogeological parameters was performed by ga, and three methods were used to evaluate groundwater resources of yangzhuang karst water system in this paper. calculation and analysis of water resources carrying capacity of yangzhuang basin were set up. as well as suggestions of protection about yangzhuang karst water system was provided clearly
在分析研究羊莊盆地水文地質條件的基礎上，應用遺傳演算法（ ga ）進行水文地質參數優選，並利用三種方法計算評價了羊莊巖溶水系統的可采資源量，計算分析了羊莊盆地的水資源承載能力，並提出了增源增采及分級保護的措施。 -
Differences of natural characteristics between two typical karst ecosystems in lijiang river basin
灕江流域典型巖溶生態系統的自然特徵差異 -
Therefor, in the light of theory and methods of karst hydrogeomorphology and the knowledge of transformation, balance and variation of matter and energy in karst drainage basin, we can examine stone forest within a specific scope of time and space, and reveal the mechanism and the development model of stone forest with the help of the principle of the mutual response processes among base - level, water flow and forms. just based on the understanding above, the paper, with a special reference to the lunan stone forest which is the best developed one in china, discusses the hydro - geomorphlogical structure of the bajiang river, geomorphological types and spacial distribution feature of the stone forest, and studies the erosion rate on the top of stone forest, soil erosion rate, sub - soil dissolution rate and their combined influences on the evolution of stone forest, furtherly brings forward and demostrates the " tri - level erosion " mechanism for the development of stone forest
正是基於這種認識，本文以我國石林發育最完美的路南石林為研究對象，研究了巴江喀斯特流域的水文地貌結構特徵、石林的形態類型及其空間分佈特徵；探討了石柱頂部的剝蝕速率（ a ） 、表土剝蝕速率（ s ） 、土下溶蝕強度（ c ）及其組合對石林發育的影響，提出並論證了路南石林發育的「三重剝蝕」機制；通過對石林發育必備條件的剖析，以及對巴江喀斯特流域演變階段的定量研究、水文地貌系統的空間耦合分析，探討了巴江喀斯特流域的演變與路南石林發育間的關系，並結合該流域的演化史，提出了巴江喀斯特流域演變與路南石林發育的模式。 -
Employing the satellite images of landsat - mss and landsat - tm and the integrated techniques of rs, gis, and gps, the authors, with maotiaohe river basin as a case, studied the process and driving factors of land use / cover changes since the beginning of 1970s, and modeled the possible land use / cover changes scenarios in the coming 10 years based on clue - s model, and then made an ecological evaluation on effect of the changes over the past 30 yeas as well as in the coming 10 years by using theory and method of landscape ecology. in this research, the authors, from the angle of international lucc studies, threw much light on the land use / cover changes in the basin and also the derived ecological and environmental problems such as karst rocky desertification
本文以位於貴州中部的貓跳河喀斯特流域為對象，以1973年的mss和1990年、 2002年的tm等衛星影像為數據源，運用rs - gis - gps集成技術，研究了該地區在過去三十年間土地利用/覆被變化的過程、驅動機制，運用clue - s模型模擬、預測了該流域在不同目標情景模式下的土地利用/覆被變化，並運用景觀生態學的方法對貓跳河流域過去三十年間的土地利用/覆被變化以及未來不同情景模式下的土地利用/覆被變化的生態效應進行了評價。 -
As a kind of karst geomorphology, stone forest is always distributed in a kast drainage basin, its development is inevitably related to evolution of the whole catchment
作為一種喀斯特地貌形態，石林總是分佈於特定的流域中，它的形成和發育演化與其所在流域的整體演化必然存在著密切的聯系，石林的出現、消亡是和流域地貌的發育演化階段相關的。 -
The characteristic study of karst water at houzhai underground basin in puding county, guizhou province
貴州普定后寨地下河流域巖溶水特徵研究 -
Study of structures and water resources development patterns in karst watershed a case study at the houzhai basin, puding, guizhou
以貴州省普定后寨巖溶流域為例 -
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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