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蒙特卡洛模型在现代黄河三角洲浅层沉积物压实速率模拟中的应用

张翼 黄海军 刘艳霞 刘一霖

海洋地质与第四纪地质2017,Vol.37Issue(2):185-191,7.
海洋地质与第四纪地质2017,Vol.37Issue(2):185-191,7.DOI:10.16562/j.cnki.0256-1492.2017.02.019

蒙特卡洛模型在现代黄河三角洲浅层沉积物压实速率模拟中的应用

APPLICATION OF MONTE CARLO MODEL TO SIMULATION OF COMPACTION RATES OF SHALLOW SEDIMENTS IN THE MODERN YELLOW RIVER DELTA

张翼 1黄海军 2刘艳霞 1刘一霖1

作者信息

  • 1. 中国科学院海洋研究所海洋地质与环境重点实验室,青岛266071
  • 2. 中国科学院大学,北京100049
  • 折叠

摘要

Abstract

The traditional methods used in the study of shallow sediment compaction,which is one of the important contributors to land subsidence,are usually based on drillings and profile measurement with local computation in the Yellow River Deltaic area.In order to overcome the methodological limitation and restriction in past studies,the Monte Carlo approach and the stratified summation method are adopted.With the borehole data obtained from the Project on Comprehensive Engineering Geological and Hydrogeological Survey in 1987,we numerically modeled the shallow sediments of the whole delta,calculated the compaction rates and analyzed the influence factors of compaction simulation.The results show that the present compaction rates vary in a range from 0.18mm/a to 9.07mm/a.The influence factors of compaction rates are mainly the geotechnical parameters,such as initial porosity and compressibility and the average net accumulation rates,both of which are significantly and positively correlated with the present compaction rates,and the soft layer is the major contributor to the sediment compaction and land subsidence.The results are fit to the history of the Yellow River delta if simulations are made for lobes with time.Combined with the ground subsidence level monitoring data,it is found that the contribution of consolidation and compaction of shallow sediments accounts for about 13% of the total settlement.

关键词

叶瓣/固结压实/蒙特卡洛模拟/现代黄河三角洲

Key words

lobe/compaction/Monte Carlo simulations/the Modern Yellow River Delta

分类

海洋科学

引用本文复制引用

张翼,黄海军,刘艳霞,刘一霖..蒙特卡洛模型在现代黄河三角洲浅层沉积物压实速率模拟中的应用[J].海洋地质与第四纪地质,2017,37(2):185-191,7.

基金项目

国家自然科学基金项目(41276082) (41276082)

海洋地质与第四纪地质

OA北大核心CSCDCSTPCD

0256-1492

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