地温梯度的英文

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用"地温梯度"造句

geothermal gradient
geothermic degree
geothermic gradient
underground temperature gradient

地温: ground temperature; earth te ...
梯度: gradient; grad
古地温梯度: paleogeothermal gradient
地温梯度钻井: geothermal gradient drilling
地热梯度；地温梯度: geothermal gradient

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Based on analysis of geologic foundation record about pingzhuang basin , a lot of sino - foreign geothermal geology record and investigation of field geology , measuring of ground temperature in person and geo - chemical analysis of ascension spring , gushing water of fault , the fact that the anomaly of geothermal gradient of pingzhuang basin , which is in region of low geothermal gradient , is caused by redistribution of conduction - oriented geothermal heat flow which is result from upheaval and depression of basin foundation bed is pointed out . after the field of ground temperature is simulated under the background of conduction - oriented geothermal heat flow by means of ansys , the characteristic of ground temperature distribution of top surface of basin foundation bed ( yixian team ) is revealed . the sound condition of transmissibility fault and feeding water source , which are imperative in formation of the low - medium temperature geothermal system of convective type , is possessed in pingzhuang basin
通过对平庄盆地基础地质资料、国内外大量地热地质资料的分析和野外地质调查、矿井实测地温以及上升泉、断层涌水的地球化学分析等工作基础上，指出地处低地温梯度背景区的平庄盆地地温梯度异常是由于盆地基底隆起和坳陷引起传导型大地热流再分配所致；运用州sys数值模拟了大地热流向地表传导背景下的盆地地温场，从而揭示了盆地基底(义县组)顶界面地温分布特征；阐明了盆地具有形成中低温对流型地热系统所必需的导水断裂、补给水源等的良好条件，中低温对流型地热系统是地热勘查的主要对象；圈定了平庄盆地北部朝阳沟?骆驼营子地热勘查远景区。
Through studying it is shown that in chagan sag , the geothermal gradients in the center are higher than those around the sag margin and major factors influencing the characteristics of temperature field distribution are the property of geotectogenesis and the differences in tectonic portion , lithology and underground water behaviour ; there are three types of mudstone compaction , i . e . normal compaction , undercompacition and overcomepaction ; there are two pressure systems in sandstone reservoirs , i . e . normal pressure and negative pressure systems and the strata ' s being uplifted and denuded is the key factor leading to the formation of the negative pressure system in reservoir ; and the distinctive temperature - pressure field characteristics in the sag are possessed of important petroleum geological significance in hydrocarbon source maturity , hydrocarbon generation , widening on oil and gas exploration domain and selecting exploration targets , etc
研究表明，查干凹陷中心的地温梯度高于凹陷边缘，大地构造性质及所处构造部位、岩性与地下水活动的差异是影响凹陷地温场分布特徵的主要因素；泥岩压实存在正常压实、欠压实和过压实三种类型，砂岩储层段压力类型可分为正常和负压两个系统，地层抬升剥蚀是导致储层负压系统形成的主导因素；凹陷独特的温压场特徵对烃源岩成熟、油气生成、油气勘探领域的扩大及勘探方向的选择等具有重要的油气地质意义。
Also the theoretical basis of the method have been checked through simple deducing simulation and the influences of various physical parameters on the method have been studied . it is shown that the method is theoretically reliable for the production oil wells without very high production rate and is more suitable in field production for oil wells ( i ) in area with bigger geothermal gradient ; ( ii ) producing fluids ( oil and water ) with distinguish thermal characteristics ; ( iii ) producing oil with lower heat capacity or water with higher heat capacity ; ( iv ) with good surface measurement accuracy , as well as the method h as certain requirements on the accuracy of the temperature and flowmeter logs sensors
就该产出剖面方法的理论基础进行了简单的正演模拟和可能影响该方法的各项物理参数进行了全面的考察，结果表明，该方法对于非高产的生产油井来说在理论上是可靠的，在实际生产中适合于( 1 ) 、油井所在地区地温梯度较大的油井； ( 2 ) 、油水热特性差别较大的油井； ( 3 ) 、油比热容值偏低水比热容值偏高的油井； ( 4 ) 、井口计量精度较高的油井，并且对井温测井和流量测井的传感性精度有一定的要求。