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云南高原湖泊表层沉积物粒度特征及环境指示意义

李华勇 张虎才 陈光杰 常凤琴 段立曾 王教元 卢慧斌 吴汉 胡葵

沉积学报2017,Vol.35Issue(3):499-507,9.
沉积学报2017,Vol.35Issue(3):499-507,9.DOI:10.14027/j.cnki.cjxb.2017.03.008

云南高原湖泊表层沉积物粒度特征及环境指示意义

The Grain Size Distribution Characteristics of Surface Sediments from Plateau Lakes in Yunnan Province and Their Environmental Significances

李华勇 1张虎才 1陈光杰 1常凤琴 1段立曾 1王教元 1卢慧斌 1吴汉 2胡葵1

作者信息

  • 1. 云南师范大学旅游与地理科学学院高原湖泊生态与全球变化重点实验室/高原地理过程与环境云南省重点实验室,昆明 650500
  • 2. 中国科学院南京地理与湖泊研究所,南京 210008
  • 折叠

摘要

Abstract

To investigate the distribution pattern and significance of grain size and provide accurate analogues for grain size records from lake cores, we analyzed surface sediments from 15 lakes of Yunnan Province, China for grain size.Meanwhile, the grain size components of the surface sediments of the 15 lakes were partitioned using the log-normal distribution function method.The results showed that frequency curves of samples indicated polymodal and consisted of two to five grain-size components with the modal size varying within ranges of 0.6~423.0 μm.These components are specified from fine to coarse modes as clay (C1), fine silt (C2), silt (C3), fine to medium sand (C4) and coarse sand (C5).The grain size analysis reveals that the C1 components were the long-term superfine dust and aerosol in the atmosphere which entered the lake water body through the process of gravity and precipitation, and may have represented the background level of atmospheric dust and aerosols in southwest China;C2 and C3 were the main components of surface sediments, the modal size of which reflected the precipitation intensity of the watershed;C4 and C5 components only appeared in minority surface sediments of lakes with the contents were extremely low, and were significantly related to the lake hydrodynamic force.For the large lakes, such as Dianchi and Fuxian Lakes, it requires two processes for the sand components to reach the central part of lakes: process of from drain basin to lakes and from lakeshore to the middle of lakes, and the second one plays a main role, affected by lake current, water depth, gradient of lake basin and so on.Under the background of the drought in southwest China, some small lakes in Yunnan shrinked and even disappeared.However, because of the decrease of precipitation and weakening of general circulation, surface runoff and hydrodynamics of lakes recede, thus the material which transmit to the center of the lakes were primarily fine grain.Small lakes located in the mountainous region, with the limited catchment area and conspicuous terrain slope, can be affected by the surface runoff directly and strongly.Therefore, the increase of coarse grain in the sediments of this kind of lakes reflected the enhancement of precipitation or the precipitation intensity.

关键词

云南/高原湖泊/表层沉积物/粒度分布特征/物源分析/沉积动力

Key words

Yunnan Province/plateau lakes/surface sediments/grain size distribution characteristics/source analysis/sedimentary dynamics

分类

天文与地球科学

引用本文复制引用

李华勇,张虎才,陈光杰,常凤琴,段立曾,王教元,卢慧斌,吴汉,胡葵..云南高原湖泊表层沉积物粒度特征及环境指示意义[J].沉积学报,2017,35(3):499-507,9.

基金项目

国家自然科学基金(41361008),云南省领军人才计划(2015HA024),云南省高端人才引进项目(2010CI111)[National Natural Science Foundation of China, No.41361008 (41361008)

Leading Talents Program of Yunnan Province , No.2015HA024 ()

Senior Talent Program of Yunnan Province, No.2010CI111] ()

沉积学报

OA北大核心CSCDCSTPCD

1000-0550

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