出露面积 meaning in Chinese
outcroarea
outcrop area
Examples
- The bareness area of carbonate rock of southwest china is 41 . 05 + 1004km2 , it is the biggest karst continuum strip
我国西南地区碳酸盐类岩石出露面积达41 . 05万km ~ 2 ，是世界上最大的岩溶连续带。 - Carbonate area gets to 41 . 05x 104 km2 in southwest china . it is the maximal continuum of karst mountain in the world . the dimensionality area is about 82 . 4 thousands km2 in chongqing region
我国西南地区碳酸盐类岩石出露面积达41 . 05x10 ~ 4km ~ 2 ，是世界上最大的岩溶连续带。 - The bareness carbonatite rock in chongqing is about 3 . 91 x 104km2 , makes up of 50 % of the overall land , and distributes mostly at northeast ( include three gorges reservoir area ) and southeast counties of chongqing
重庆市碳酸盐岩出露面积约3 . 91万km ~ 2 ，约占幅员总面积( 8 . 24万km ~ 2 )的50 ，主要集中分布于渝东北(其中包括三峡库区)和渝东南各区市县。 - Abstract : according to the base flow separation results from hydrographs in many watershed , the best regression equation expressing the relationship between annual precipitation infiltration coefficient and the weight of different strata area to total area of the watershed is established . the equation can be used to calculate the precipitation infiltration recharge for different ground water basins in which the strata distribution and the precipitation are given . the precipitation recharge is equivalent to the ground water recharge in some mountainous area where the exploitation of ground water resources are far from being sufficient
文摘:降水入渗补给系数与地层相关分析的目的，是为推求山丘区降水入渗补给量.鲁中山丘区是由各种不同地层出露组成的山丘区域.在多个水文流域基流分割基础上，建立流域年均降水入渗补给系数与各种地层出露面积占流域总面积权重间的最佳回归方程，利用该回归方程和地层分布及降水量推算不同地下水流域的降水入渗补给量.在地下水开发利用不高的山丘区，降水入渗补给量即为地下水补给量 - Limestone and dolomite cover about 130 km2 which takes up about 1 / 7 areas of the national land in china . besides , it is pluviose , muggy and damp in there areas , all of these accelerate the karst caves . there are more than 100 , 000 caves and holes under the earth , which consists of a karst caves kingdom in the world
中国石灰岩和白云岩的出露面积约为130km2 ，约占全国总面积的1 7 ，加之雨量充沛，气候温热潮湿，喀斯特较为发育，地下洞穴孔道，计有数十万个之多，成为世界上的洞穴王国。