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   补给温度 的翻译结果: 查询用时:0.501秒
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补给温度
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  supply temperature
     The new method of determining groundwater supply temperature and rainfall by dissolved noble gases
     测定地下水补给温度与降雨量的最新方法——惰性气体法
短句来源
     Groundwater supply temperature and rainfall are important parameters to hydrogeology,but we just get their relative changes by existing methods in almost moment.
     地下水补给温度与降雨量是重要的水文地质参数,已有的测定方法大多只能给出其相对变化。
短句来源
     The new method of determining groundwater supply temperature and rainfall by dissolved noble gases is discussed.
     本文介绍的惰性气体法能同时求得地下水补给温度与降雨量的值,其基本原理是:利用地下水中惰性气体的平衡溶解量计算出地下水补给温度;
短句来源
  相似匹配句对
     T is temperature, ℃.
     T为温度,℃。
短句来源
     Measure of Temperature
     温度的测量
短句来源
     The new method of determining groundwater supply temperature and rainfall by dissolved noble gases
     测定地下水补给温度与降雨量的最新方法——惰性气体法
短句来源
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  supply temperature
Achieving the minimum chilled water supply temperature leaving each chiller.
      
All fresh air was transported directly into the air heater, where was heated up to required supply temperature.
      
Based on the outside air conditions at night, the supply temperature of glycol chilled water can be increased.
      
Based on the outside air conditions at night the supply temperature of chilled water can be increased.
      
Chilled water supply temperature shall be reset in accordance with Section 1432.2.2.
      
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The Disciplinarian of inorganic nitrogen content in typical reservoirs and lakes yearly and monthly evolution is derived based on the continuously environmental and hydrological monitor between 1992 and 1997 in Jilin Province, the cause of formation and the relations between the inorganic nitrogen content and other indexes also discussed. Most of the lakes and Reservoir are at the phase of medium eutrophication and the lakes in city are at the higher. eutrophication. Because of the extra origin supply, temperature...

The Disciplinarian of inorganic nitrogen content in typical reservoirs and lakes yearly and monthly evolution is derived based on the continuously environmental and hydrological monitor between 1992 and 1997 in Jilin Province, the cause of formation and the relations between the inorganic nitrogen content and other indexes also discussed. Most of the lakes and Reservoir are at the phase of medium eutrophication and the lakes in city are at the higher. eutrophication. Because of the extra origin supply, temperature and the function of lakes, the seasonal evolutions of inorganic nitrogen are different and the total nitrogen changes undualtely in a year. The inorganic nitrogen and total nitrogen increase year by year. Being affected by all kinds of factors of water quality, the relations between the content of inorganic nitrogen and other water quality indexes are little.

通过对吉林省典型湖库 1992— 1997年的连续水质水文监测 ,探讨了吉林省主要湖库中无机氮含量的季节变化、年际变化规律及其成因 .吉林省大多数湖库中的总氮处于中等富营养化程度 ,城市湖库 (南湖 )已超过富营养水平下限 .受到外源性补给、温度和湖库使用功能的影响 ,湖库中各类型无机氮含量季节变化不一 ,总氮在全年出现波状起伏变化 .大多数湖库中的无机氮和总氮出现逐年增加的趋势 .湖库中无机氮含量受到水体中各种水质因素的综合作用 ,与其它单个水质参数之间的关系不明显

Groundwater supply temperature and rainfall are important parameters to hydrogeology,but we just get their relative changes by existing methods in almost moment.The new method of determining groundwater supply temperature and rainfall by dissolved noble gases is discussed.The groundwater supply temperature value can be worked out with the volume of balance dissolving noble gas in groundwater,but the rainfall value can be worked out with the volume of overmuch dissolving noble gas on the basis of getting groundwater...

Groundwater supply temperature and rainfall are important parameters to hydrogeology,but we just get their relative changes by existing methods in almost moment.The new method of determining groundwater supply temperature and rainfall by dissolved noble gases is discussed.The groundwater supply temperature value can be worked out with the volume of balance dissolving noble gas in groundwater,but the rainfall value can be worked out with the volume of overmuch dissolving noble gas on the basis of getting groundwater supply temperature.And this method is mainly adaped to deep groundwater in closed condition.

地下水补给温度与降雨量是重要的水文地质参数,已有的测定方法大多只能给出其相对变化。本文介绍的惰性气体法能同时求得地下水补给温度与降雨量的值,其基本原理是:利用地下水中惰性气体的平衡溶解量计算出地下水补给温度;在得到地下水补给温度的基础上,利用地下水中惰性气体的“过剩空气”量计算出降雨量。该方法主要适用于封闭条件下的深层地下水。

 
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