Development of Direct Measurement Technics for Thermophysical Properties of Rock Mass in situ by Well Logging
Development of Direct Measurement Technics for Thermophysical Properties of Rock Mass in situ by Well Logging
批准号:
09555318
负责人:
KIYOHASHI Hiroshi
金额:
$3.78万
依托单位:
依托单位国家:
日本
项目类别:
Grant-in-Aid for Scientific Research (B)
财政年份:
1997
资助国家:
日本
项目状态:
已结题
起止时间:
1997 至 1999
中文摘要
Thermophysical properties of deep reservoir rocks应该直接监测一个方法technique in situ,because their values by laboratory measurements using samples might be influenced due to theintracrystalline microcracks originating from a stress released from the核心驱动程序。作者已开发了一种新的方法和系统,用于simultaneous measurements of The thermalconductivity, thermal diffusivityand the specific heat of rocks in situ at temperatures from 273 to 473k, by applying the transient,hot-wire comparative method. In this study, a hot wire with diameter, d=8050或30μm and length=50mm was inlaid in the center of the surface of the substrate (elastic silicon)gum plate of 40mm×90mm×10mm) used as a reference material. Three K-thermocouples, T - 20 D2,T - D21 d - 2 and T - D22 d - D2 of diameter d[μm] were inlaid at x - D20 d - 2,x - D21 - D2 and x - D22 - D2[mm] from center of the hot wire, respectively,in the surface. Temperature rise Δθ D20…More at x D20 D2and the temperature difference Δθ D212 - D2=(θ D21 - D2)-θ D22 - D2 between θ D21 - D2 atD21 - D2 and θ D22 - D2 at x - D22 - D2 against logarithmic time ln(t) and 1/(t), respectively,were used in the thermal conductivity, λ D2s - D2, and the thermal diffusivity,α - D2s - D2,这个方法是适用于flat boundary surface of half infinite body ofthe sample whose thermal conductivity is λ D2FS D2 (=λ D2s D2).In the study,the effect of a ratio of the curvature radius of a borehole R[mm]=D/2diameter) to the radius of the hot wire, r=d/2,and the ratio to the reference thermal conductivity of the substrate, λ D2R D2,to the sample thermal conductivity of the rocks in situ, λ D2s D2,on measurement values for curved boundary surface of the borehole, λ D2cs D2,was studied to evaluate the values of λ D2s D2. Model boreholes from 66 to 120mm in diameter weredrilled in each several blocks of rocks having different values of λ D2s D2. Six types of sensorsinlaying the hot wire and the thermocouples having different diameters, d[μm] of 80,50 and 30 were used. The inlaid positions of x D20 D2,x - D21 - D2和x - D22 - D2 were fixed at 0.5, 2.0和4.0 mm, respectively.As the results,suitable design parameters被订购以评估thermal条件,2. If the measured λ-values on the curved boundary surface in the borehole drilled intothe subsurface material having λ D2FS D2 were λ D2CS D2,the ratio of (λ D2CS D2/λ D2FS D2) were less than +10% for the ratios larger than D/ D =2400,and less than +5% for the ratios larger than D/ D =3000, respectively,without dependency of the ratio of (λ D2S - D2/λ D2R - D2). Probes of prototype No.1 of whichsubstrates were made by synthetic rubber for boreholes having diameter D= 116to 120mm were designed。substrates are pressurized by compressed air or hydraulic oilafter the probes been inserted into the borehole. Less
英文摘要
Thermophysical properties of deep reservoir rocks should be directly obtained by a measurement technique in situ, because their values by laboratory measurements using samples might be influenced due to the intracrystalline microcracks originating from a stress released from the core during the drilling. The authors have developed a new method and system for simultaneous measurements of the thermal conductivity, the thermal diffusivity, and the specific heat of rocks in situ at temperatures from 273 to 473K, by applying the transient, hot-wire comparative method. In this study, a hot wire with diameter, d=80, 50 or 30μm and length=50mm was inlaid in the center of the surface of the substrate (elastic silicon gum plate of 40mm×90mm×10mm) used as a reference material. Three K-thermocouples, TィイD20ィエD2, TィイD21ィエD2 and TィイD22ィエD2 of diameter d[μm] were inlaid at xィイD20ィエD2, xィイD21ィエD2 and xィイD22ィエD2[mm] from center of the hot-wire, respectively, in the surface. Temperature rise ΔθィイD20ィエD2 … More at xィイD20ィエD2, and the temperature difference ΔθィイD212ィエD2=(θィイD21ィエD2)-θィイD22ィエD2) between θィイD21ィエD2 at xィイD21ィエD2 and θィイD22ィエD2 at xィイD22ィエD2 against logarithmic time ln(t) and 1/(t), respectively, were used in calculation of the thermal conductivity, λィイD2sィエD2, and the thermal diffusivity, αィイD2sィエD2, respectively. Originally this method is applied for flat boundary surface of half infinite body of the sample whose thermal conductivity is λィイD2FSィエD2 (=λィイD2sィエD2).In the study, the effect of a ratio of the curvature radius of a borehole, R[mm]=D/2 (D: diameter) to the radius of the hot wire, r=d/2, and the ratio to the reference thermal conductivity of the substrate, λィイD2RィエD2, to the sample thermal conductivity of the rocks in situ, λィイD2sィエD2, on measurement values for curved boundary surface of the borehole, λィイD2csィエD2, was studied to evaluate the values of λィイD2sィエD2. Model boreholes from 66 to 120mm in diameter were drilled in each several blocks of rocks having different values of λィイD2sィエD2. Six types of sensors inlaying the hot-wire and the thermocouples having different diameters, d[μm] of 80, 50 and 30 were used. The inlaid positions of xィイD20ィエD2, xィイD21ィエD2 and xィイD22ィエD2 were fixed at 0.5, 2.0 and 4.0 mm, respectively.As the results, suitable design parameters were obtained in order to evaluate the thermal conductivity, λィイD2FSィエD2. If the measured λ-values on the curved boundary surface in the borehole drilled into the subsurface material having λィイD2FSィエD2 were λィイD2CSィエD2, the ratio of (λィイD2CSィエD2/λィイD2FSィエD2) were less than +10% for the ratios larger than D/d=2400, and less than +5% for the ratios larger than D/d=3000, respectively, without dependency of the ratio of (λィイD2SィエD2/λィイD2RィエD2). Probes of prototype No.1 of which substrates were made by synthetic rubber for boreholes having diameter D=116 to 120mm were designed. The substrates are pressurized by compressed air or hydraulic oil, after the probes have been inserted into the borehole. Less
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幾世橋広: "岩盤熱物性値のボアホール計測技術の開発-円孔壁面を用いる方法-"資源・素材学会春季大会講演集(I)資源編1999,3,29〜31,東京. 149-150 (1999)
Hiroshi Ikusehashi:“岩石热物理性质钻孔测量技术的发展 - 使用圆形孔壁的方法”日本自然资源与材料学会春季会议论文集(I)资源版1999年,3,29-31,东京149。 -150 (1999)
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Hiroshi Kiyohashi: "Development of Direct Measurement Method for Thermophysical Properties of Reservoir Rocks in situ by Well Logging"Proceedings of World Geothermal Congress 2000, Kyushu-Tohoku, Japan, 2000. (査読済み,掲載予定). (2000)
Hiroshi Kiyohashi:“通过测井直接测量储层岩石热物理性质的方法”,2000 年世界地热大会论文集,日本九州东北部,2000 年。(同行评审,待出版)。
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Hiroshi Kiyohashi: "Evaluation of Thermal Conductivity of Granitoid Stratum at Deep Depths by Core Samples"High Temperature-High Pressure. 32(査読済み,掲載予定). (2000)
Hiroshi Kiyohashi:“通过岩心样品评估深部花岗岩地层的热导率”32(同行评审,待出版)。
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幾世橋 廣: "岩盤熱物性値のボアホール計測技術の開発-基礎実験(3)と原型1号プローブの試作-"(社)資源・素材学会平成12年度春季大会研究業績発表講演要旨集. (一般発表)2210. (2000)
Hiroshi Ikusehashi:“岩石热物理性质的钻孔测量技术的开发 - 基础实验(3)和原型 1 号探测器 -” 日本自然资源与材料学会 2000 年春季会议上发表的研究结果摘要集(。一般公告)2210。(2000)
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Hiroshi, KIYOHASHI: "Evaluation of Thermal Conductivity of Granitoid Stratum at Deep Depths by Core Samples"High Temperature-High Pressure. Vol.32(in press). (2000)
Hiroshi,KIYOHASHI:“通过岩芯样品评估深部花岗岩地层的导热系数”高温高压。
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共 6 条
FUNDAMENTAL STUDIES ON ICE ABRASIVE JETS
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批准号:06651092
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项目类别:Grant-in-Aid for General Scientific Research (C)
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资助金额:$1.34万
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财政年份:1994
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负责人:KIYOHASHI Hiroshi
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依托单位:
海外基金