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循环深度
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  circulation depth
     The estimated circulation depth of the hot water ranges from 1500-2000 meters.
     阐明了地下热水的入渗途径,其循环深度1500—2000m。
短句来源
     Based on hydrogen and oxygen isotope study,the origin,recharge as well as the temperature,circulation depth and mixing proportion of geothermal waters in Guanzhong area were analyzed.
     通过对关中南部地下热水氢氧同位素组成研究,探讨了研究区地下热水的起源、补给以及有关净热水的循环温度、循环深度、与冷水混合比例等与地下热水有关的热点问题,并与传统水文地质勘探方法进行了对比研究。
短句来源
     CIRCULATION DEPTH OF THE THERMAL WATER IN ZHANGZHOU GEOTHERMAL FIELD
     漳州热田地下热水的循环深度
短句来源
     A DISCUSSION ON THE RELATION OF CIRCULATION DEPTH OF HOT SPRING WATER TO SEISMIC ACTIVITY ON THE NORTHERN SEGMENT OF THE HONGHE FAULT ZONE
     红河断裂带北段温泉水循环深度与地震活动性的关系探讨
短句来源
     Heat reservoir temperature of water samples collected from 14 hot springs on the northern segment of the Honghe fault zone is calculated by using SiO2-geothermometer, and in connection with local geothermal gradients, circulation depth of the hot spring waters is also calculated. Meanwhile, frequency and focal depth of earthquakes occurring from 886 to 1987 are counted up and analysed.
     利用SiO_2地热温标计算了红河断裂带北段14个温泉水的热储温度,并结合当地地温梯度计算了温泉水的循环深度,同时统计分析了886~1987年间的地震频度和震源深度。
短句来源
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  “循环深度”译为未确定词的双语例句
     The depth of main circulation of underground water is1—3km.
     地下水的主要循环深度在1—3公里。
短句来源
     The thermal groundwater is estimated to circulate at 2792.45 m depth.
     估算热水循环深度为2792.45m。
短句来源
     A linear equation concerning the rainfall mass curve, δD(‰) =8.8δ~(18)0(‰) +18.1, was derived from the hydrogen/oxygen isotopic data.
     通过氢氧稳定同位素的研究,建立了福州地区的雨水线,其线性方程为:δD(‰)=8.8δ18O(‰)+18.1,并论证福州地下热水的成因是由大气降水补给,经深循环加热形成的,其循环深度约3500米。
短句来源
     2. According the principle of geothermy increasing, the Binglingshan spring-water cycle depth is 640m.
     2.利用地热增温原理估算得出,冰凌山泉水循环深度为640m。
短句来源
     According to the coincidence between focal depth and the depth of groundwater cycle, it thinks that the induced earthquakes in the reservoir resulted from a sudden increase of pore water pressure which is caused by the permeance of water to the reservoir.
     根据震源深度与地下水循环深度吻合,认为水向库基深层渗透导至水库基岩石孔隙压骤增是本库诱发地震的主因。
短句来源
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  相似匹配句对
     The thermal groundwater is estimated to circulate at 2792.45 m depth.
     估算热水循环深度为2792.45m。
短句来源
     CIRCULATION DEPTH OF THE THERMAL WATER IN ZHANGZHOU GEOTHERMAL FIELD
     漳州热田地下热水的循环深度
短句来源
     RECYCLE
     循环再利用
短句来源
     The Doming cycle
     “Deming”循环
短句来源
     Speed and depth;
     速度和深度;
短句来源
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  circulation depth
Determining the circulation depth of thermal springs in the southern Rocky Mountain Trench, south-eastern British Columbia, Cana
      


Temperature distribution along the wellbore is of significant importance in producing highly viscous and waxy crudes. Hot fluid circulation in well will increase temperature level and improve crudes mobility. In this paper various circulation programs are suggested and discussed from heat transfer calculation. The effect of circulation rate, thermal properties, circulating depth and initial temperature of hot fluid on temperature distribution has been obtained.

沿井筒的温度分布对高粘度、高含蜡原油的生产具有很大的意义。热流体循环将提高井筒中的温度水平并改善原油的流动性。本文提出了几种不同的循环方案并根据传热计算作了探讨,得到了热流体循环量、热物性、循环深度和初温度对温度分布的影响。

On the estimating method of silica heat flow value proposed byC·A·Swanberg and P.Morgan,this paper adopts the content of SiO_2of 1269 underground water samples in Fujian,and calculates thetemperature and silica heat flow value when SiO_2 in solution isequaled.It has been indicated from the calculated results that inthe western part of Fujian,namely the west of Zhenghe—Dapu,silica heat flow value is lower than the heat flow mean(1.5HFU)in the terrene,while in the east of Zhenghe-Dapu,namely theFujian-Taiwan shovellike...

On the estimating method of silica heat flow value proposed byC·A·Swanberg and P.Morgan,this paper adopts the content of SiO_2of 1269 underground water samples in Fujian,and calculates thetemperature and silica heat flow value when SiO_2 in solution isequaled.It has been indicated from the calculated results that inthe western part of Fujian,namely the west of Zhenghe—Dapu,silica heat flow value is lower than the heat flow mean(1.5HFU)in the terrene,while in the east of Zhenghe-Dapu,namely theFujian-Taiwan shovellike active fault,the silica heat flow value is slightly higher than the heat flow mean in theterrene.The valueis about 2HFU,belonging to heat flow area of weakly positiveanomaly.The depth of main circulation of underground water is1—3km.

本文根据斯旺勃格和摩根所提出的硅热流值估算方法,利用福建全省已有的1269个地下水样中的二氧化硅含量,计算了水溶液二氧化硅达到平衡时的温度和硅热流值。计算结果表明,福建西部印政和—大埔一线以西硅热流值都低于地球表面的平均热流值(1.5HFU),而在政和—大埔以东地区,即闽台铲状活动断裂之上,硅热流值略高于地表平均热流值,达(2HFU)左右,属于微弱正异常热流区。地下水的主要循环深度在1—3公里。

According to the tectonic framework in Fujian coastal area, based on analysing the character of local geological structure in Zhangzhou basin, the character of geothermal field indications, the dynamical variations of hydro-thermal elements, and chemical components of hot water in different depth, the paper indicates that the heat source in the area is due to reactivation of the ancient fault, the main source of the hot water is rainfall, and further illustrates the pathway of the hot water. The estimated circulation...

According to the tectonic framework in Fujian coastal area, based on analysing the character of local geological structure in Zhangzhou basin, the character of geothermal field indications, the dynamical variations of hydro-thermal elements, and chemical components of hot water in different depth, the paper indicates that the heat source in the area is due to reactivation of the ancient fault, the main source of the hot water is rainfall, and further illustrates the pathway of the hot water. The estimated circulation depth of the hot water ranges from 1500-2000 meters. Finally the general direction for further exploration and excavation of underground hot water is proposed.

本文依据福建沿海一带大地构造情况,在分析了漳州盆地局部地质构造特征、地温场显示特征、地下热水的动态变化以及不同深度地下热水的化学组分之后指出:漳州地热区主要热源来自老断裂的重新活动,地下热水的来源主要是大气降水。阐明了地下热水的入渗途径,其循环深度1500—2000m。结合成因分析,为今后进一步勘探和开发地下热水提出了总体方向。

 
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