| 南海北部神狐海域天然气水合物分解的测井异常 |
| |
| 引用本文： | 王秀娟,吴时国,王吉亮,杨胜雄,王真真.南海北部神狐海域天然气水合物分解的测井异常[J].地球物理学报,2013,56(8):2799-2807. |
| |
| 作者姓名： | 王秀娟 吴时国 王吉亮 杨胜雄 王真真 |
| |
| 作者单位： | 1. 中国科学院海洋地质与环境重点实验室, 中国科学院海洋研究所, 青岛 266071;
2. 国土资源部海洋油气资源与环境地质重点实验室, 青岛 266071;
3. 中国科学院大学, 北京 100049;
4. 广州海洋地质调查局, 广州 510075 |
| |
| 基金项目： | 国家自然科学基金，国土资源部海洋油气资源与环境地质重点实验室基金，国家重点基础研究发展计划(973计划) |
| |
| 摘 要： | 南海北部神狐海域GMGS-1钻探揭示SH3井天然气水合物位于稳定带上部,厚度约为10 m.氯离子异常计算的水合物饱和度最高达26%,高水合物饱和度层出现高电阻率和低纵波速度.为分析该低纵波速度异常,本文基于简化的三相介质理论计算了饱和水纵波速度,在深度195 m附近,测量的纵波速度小于饱和水纵波速度.利用阿尔奇公式,基于原位温度、盐度、密度孔隙度和测量的电阻率,利用交会分析确定了该井的阿尔奇常数为a=1.1和m=2.3.基于该参数,利用阿尔奇方程计算的水合物饱和度占孔隙空间5%~20%,局部地层水合物饱和度达26.8%,在垂向上分布不均匀.由于钻探可能导致水合物发生分解而产生游离气,原位游离气和水合物分解产生的气体都能造成低纵波速度异常.由于地震资料采集在测井之前完成,利用不同速度制作合成地震记录并与地震资料进行对比,能够确定水合物稳定带上部的低速异常形成原因.
|
| 关 键 词： | 天然气水合物 饱和度 分解 纵波速度 神狐海域 |
| 收稿时间： | 2012-07-12 |
Anomalous wireline logging data caused by gas hydrate dissociation in the Shenhu area, northern slope of South China Sea |
| |
| WANG Xiu-Juan
,
WU Shi-Guo
,
WANG Ji-Liang
,
YANG Sheng-Xiong
,
WANG Zhen-Zhen.Anomalous wireline logging data caused by gas hydrate dissociation in the Shenhu area, northern slope of South China Sea[J].Chinese Journal of Geophysics,2013,56(8):2799-2807. |
| |
| Authors: | WANG Xiu-Juan WU Shi-Guo WANG Ji-Liang YANG Sheng-Xiong WANG Zhen-Zhen |
| |
| Institution: | 1. Key Laboratory of Marine Geology & Environment, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China;
2. Key Laboratory of Marine Hydrocarbon Resources and Environmental Geology, Ministry of Land and Resources, Qingdao 266071, China;
3. University of Chinese Academy of Sciences, Beijing 100049, China;
4. Guangzhou Marine Geological Survey, MLR, Guangzhou 510075, China |
| |
| Abstract: | During the gas hydrate drilling expedition, GMGS-1 indicated that gas hydrate was discovered above the gas hydrate stability zone with a thickness of 10 meters at site SH3 in the Shenhu area, the northern slope of South China Sea. Gas hydrate saturations derived from observed pore-water chloride values in core samples reach the highest value of 26% in the pore space. Higher resistivity, lower P-wave velocity and slightly increasing density were identified. To explain the lower P-wave velocity, the Simplified Three-Phase Biot-type Equation (STPBE) was used to calculate the water-saturated P-wave velocity. At the depth of 195 m, the P-wave velocity from wireline logging is lower than that of the water-saturated velocity of the normal sediments. The Archie's parameters used to calculate gas hydrate saturation from resistivity were defined from the cross plot between density porosity and formation factor. Gas hydrate saturation estimated from resistivity using Archie equation with a=1.1 and m=2.3 is about 5%~20% of the pore space, with a maximum value of 26.8%, which shows that the distribution of gas hydrate is heterogeneous in vertical. The dissociation of gas hydrate (the mixture of free gas and water) may be caused by drilling. Either the in-situ free gas or gas released from gas hydrate dissociation can cause the low well-log P-wave velocity. Because surface seismic data were acquired before drilling, synthetic seismograms generated using different P-wave velocities were compared with the seismic data, which can be used to identify the cause of the low P-wave velocity observed in the well log. |
| |
| Keywords: | Gas hydrate Saturation Dissociation P-wave velocity Shenhu area |
| 本文献已被 CNKI 万方数据 等数据库收录！ |
| 点击此处可从《地球物理学报》浏览原始摘要信息 |
| 点击此处可从《地球物理学报》下载免费的PDF全文 |
|
