一种新的压实校正法

2000年 22卷 第2期
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A NEW METHOD FOR COMPACTION CORRECTION
李绍虎 吴冲龙 吴景富 何大伟
LI Shao-hu WU Chong-long WU Jing-fu HE Da-wei
中国地质大学资源学院, 湖北武汉 430074 2. 海洋石油勘探开发研究中心, 河北高碑店 074010
China University of Geosciences, Wuhan, Hubei 430074, China 2. China Offshor Oil Exploration and Development Research Center, Hebei 074010, China
根据压实前后压实曲线的相似性及单调性,设定古孔隙度-深度、古密度-深度函数,结合压实前后地层骨架体积不变、骨架质量不变原理.建立回剥压实校正方程,从而恢复地层古厚度及地层古密度,并且保证压实前后地层骨架密度不变。
According to the similarity and the monotonic characteristics of the compaction curves between the compacted and the decompacted states,the paleo-porosity-depth function φ'(Z) and the paleo-density-depth function ρ'(Z) was supposed.By using the principle which formation grain volume and mass have been keeping constant,the compaction correction equations has been established. Further,the decompacted thickness S and the average paleo-density ρs can be calculated and the grain density of the compacted and decompacted states can be kept constant.
压实校正; 体积; 质量; 相似性; 单调性;
compaction correction; grain volume keeping constant; grain mass keeping constant; similarity; monotonic increasing and decreasing;
国家自然科学基金(49732005);国土资源部定量预测及勘查评价开放实验室基金
https://doi.org/10.11781/sysydz200002110