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Fractal Characteristics of Grain Size from Zhifu Section in Yantai Area of Shandong, China and Their Environmental Significance(PDF)

《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

Issue:
2019年第05期
Page:
592-603
Research Field:
水资源与环境
Publishing date:

Info

Title:
Fractal Characteristics of Grain Size from Zhifu Section in Yantai Area of Shandong, China and Their Environmental Significance
Author(s):
LI Wu-biao1; 2;  LI Zhi-wen1; 2*;  WANG Zhi-gang1; 2;  LI Zi-kang1
(1. School of Earth Sciences, East China University of Technology, Nanchang 330013, Jiangxi, China; 2. State Key Laboratory of Nuclear Resources and Environment, East China University of Technology, Nanchang 330013, Jiangxi, China)
Keywords:
grain size;  fractal dimension;  loess;  paleosol;  last interglacial period;  last glacial period;  climate change;  Shandong
PACS:
P588.23; P512.2
DOI:
-
Abstract:
The sedimentary sequences superimposed by loess and paleosol are widely distributed in the northern of Shandong peninsula. Based on the field investigation and photoluminescence dating, the grain size and the characteristics of fractal dimension of loess sediments from Zhifu island in Yantai area of Shandong were calculated by graphical method and power exponential function method, and Late Pleistocene climate environment and evolution in the northern of Shandong peninsula were studied. The results show that the formation age of Zhifu section is 62.85-124.90 ka B.P., corresponding to last glacial-last interglacial periods, and is composed of sandy loess, loess and paleosol; the sediment from Zhifu section has a good fractal structure, which can clearly distinguish the paleosol(the fractal dimension is 2.379), loess(2.194), and sandy loess-loess(2.157); the fractal dimension has a significant positive correlation with the standard deviation, the correlation coefficient is 0.889 4; it has a high positive correlation with the average grain size and a low correlation with the kurtosis and skewness; the fractal dimension of sediment from Zhifu section show remarkable variations in alternation of peaks and valleys vertically, which can be used as an indicator of sedimentary environment; the low fractal dimension reflects the dry and cold climate, and the winter wind is strong and loess accumulation accelerates, on the contrary, the climate is warm and humid, and the paleosol is developed.

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Last Update: 2019-09-19