泉群的英文

• cluster of springs
• spring group

• "群"英文翻译    crowd; group
• "热泉群" 英文翻译 :    hot springs; hot-spring complex
• "水泉群落" 英文翻译 :    crenium
• "温泉群落" 英文翻译 :    thermium
• "交替活动的间歇泉群" 英文翻译 :    alternating geysers
• "泉群最小流量比拟法" 英文翻译 :    spring group minimum flow analogy method
• "泉泉水族" 英文翻译 :    quan quan aquarium
• "泉三" 英文翻译 :    senzo
• "泉区" 英文翻译 :    izumi-ku, sendai; izumi-ku, yokohama
• "泉山" 英文翻译 :    izuyama; xertu alin
• "泉丘" 英文翻译 :    spring dome; spring mound
• "泉山华步里" 英文翻译 :    kahori izumiyama
• "泉庆有限公司" 英文翻译 :    chuan ching co., ltd
• "泉山香织" 英文翻译 :    kaori izumiyama
• "泉桥" 英文翻译 :    izuhashi; izumibashi; izumihashi

• In 1990 ' s , the groundwater withdrawals just concentrated in urban , eastern and western suburb areas had reached 50 - 60x 104 / d . since the first breaking of jinan well complex in 1973 , the environmental quality and local people ' s daily life has seriously influenced
  济南泉群自1973年首次出现断喷以来，历时不断加长，给济南市的环境质量和城市居民生活造成了严重影响。
• Third , five schemes based on the combination different precipitation and pumping quantity is applied to the model prediction to predict the water laver in springs zone and high - point groundwater quantity exploited in 2010
  本通过对多种岩溶地下水开采方案预报对比，协调处理互为矛盾的“保泉”和“供水”目的，最终预报济南市泉群地下水位标高，确定岩溶地下水的开采方案。
• With development of the economy , groundwater in the jinan springs zone was exploited increasingly , and water level was so low that springs ca n ' t spurted any longer , even not at all in whole year . how to restore the scenery of springs spurting has been hotspot issue and aim for governments and scholars
  闻名中外的济南市趵突泉、黑虎泉等著名泉群自1970年后出现断流后，继而发展到全年断流，恢复济南泉涌名胜景观，成为各级政府和学者共同关心的热点课题。
• The paper selects the subject entitled " the isoparametric finite - element three - dimension groundwater ( fe3dgw ) model for fracture - karst water resources and numerical simulation in jinan springs zone " , which is one sub - task of items on " exploitation and springs protection of jinan fracture - karst water ( no . 200001 ) " in this paper , the following questions are discussed : first , according to the site survey , and other relative datum , the condition of physical geography , geography and hydrogeology are summarized
  本文的研究课题? ?济南市岩溶地下水数值模拟研究是山东省计委计划项目“济南市岩溶地下水开发利用与泉群保护研究( no . 200001 ) ”的子课题。主要研究内容有：第一，在调查和阅读分析相关资料的基础上，概要总结和阐述泉群研究区域的自然地理、水文地质条件和地质概况，提出研究区水文地质概念模型，进一步建立济南泉群研究区非均质各向异性三维非稳定流数学模型，利用等参有限元技术进行数值求解。
• 2 . based on the analysis of the historical evolution of jinan springs ' spurting , a quantity equation between the anaual average spring discharge and the anaual lowest water table is built according to the statistic data , which enable us to gain the corresponding relation between baseline water level and the smallest scenic discharge of spring gushing . then the groundwater discharge in the spring area is calculated and the controlling parameter of maximum available amount of groundwater exploiting is obtained
  泉域总面积1486平方公里。 (二)通过分析济南市泉群喷涌历史统计资料，首先建立泉群年平均喷涌量与年最低地下水位之间的定量方程，得出四大泉群喷涌的底限水位与最低景观流量的对应关系，然后，计算泉域内地下水的入渗补给量，再得出保证泉涌的地下水最大允许开采量的控制性参数。
• Could there exist another possibility for the south boundary of the system as follow : the rainfall infiltrates in the outcrop carbonate - mountain area of western , and moves towards south and deeper along carbonate rocks , then moves upper through the overlain tertiary system ( n ) with a thickness of 400m ( instead of running off to the springs and yellow river through a long approach of least hydraulic gradient ) , and then mainly transforms into the horizontal drainage in the loess layer of quaternary , finally drains in lu - botan depres sion
  并且提出，关于对系统南界的认识，是否存在另一可能：即在西部碳酸盐岩裸露区大气降水入渗后，沿碳酸盐岩向南向深部运动，然后，并非在极小的水力坡度驱动下长距离地向东部黄河、泉群径流排泄，而是通过上覆厚度约400m的第三系向上运动，继而主要在第四系黄土层中转为向南水平排泄到卤泊滩。