|Table of Contents|

Characteristics of Macroelements and Revealed Evolution of Weathering Intensity inSediments of Chaohu Lake, Anhui, China(PDF)

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

Issue:
2024年第06期
Page:
758-774
Research Field:
沉积地质与油气勘探
Publishing date:

Info

Title:
Characteristics of Macroelements and Revealed Evolution of Weathering Intensity inSediments of Chaohu Lake, Anhui, China
Author(s):
LI Chen-chen1; 2; 3;  WU Li2; 3*;  MAO Long-jiang4;  MA Chun-mei5;  GUAN Hou-chun6
(1. Institute of Science and Technology Historyand Meteorological Civilization,Nanjing University of Information Science & Technology,Nanjing 210044,Jiangsu, China; 2. School of Geography and Tourism, Anhui Normal University, Wuhu 241002,Anhui, China; 3. Provincial Key Laboratory of EarthSurface Processesand Regional Response in theYangtze-Huaihe River Basin, Anhui NormalUniversity, Wuhu 241002, Anhui, China; 4. School of MarineSciences,Nanjing University ofInformation Science &Technology,Nanjing 210044, Jiangsu,China; 5. School ofGeography and Ocean Science,Nanjing University,Nanjing210023,Jiangsu, China; 6. GeologicalSurvey ofAnhui Province, Hefei 230001, Anhui, China)
Keywords:
Holocene;  weathering intensity;  environmental evolution;  climate event;  influencing factor;  major element;  AMS 14C dating;  Chaohu Lake
PACS:
P512.1+2; P595
DOI:
10.19814/j.jese.2024.02005
Abstract:
Holocene is an important period for the formation and development of human civilization.Study onthe laws of climate change since Holocene will help to understand global climate change and scientifically respond to abrupt events. The major elementcontents and ratio characteristics in core SZK1507 of Chaohu Lake were conducted; combined with AMS 14C dating, the evolution process of weathering intensity in Chaohu Basin since 10.8 cal. ka B.P. was rebuilt, and the process of climate and environmental change in the basin and possible climate abrupt events were revealed, while the possible influencing factors of chemical weathering intensity were preliminarily explored. The results show that ① the valley values ofenvironmental substitution index, such aschemical index of alteration(CIA)and Ki, as well as the peak values of Ba and w, both appear in the sand layers and silt layers, indicating that the chemical weathering degree is weaker than that of other layers. ② During the period I(10.8-9.9 cal. ka B.P.)and the period Ⅲ(9.3-5.7 cal. ka B.P.), the chemical weathering intensity is strong; and weaker chemical weathering intensity occurs in the period Ⅱ(9.9-9.3 cal. ka B.P.); during the period Ⅳ(5.7-2.3 cal. ka B.P.), the chemical weathering intensity gradually weakens; during the period Ⅴ(from 2.3 cal. ka B.P. to the present), the chemical weathering intensity changes frequently, showing an overall weakening feature; in addition, there is a good consistency between the intensity of chemical weathering and climate change, revealing that Chaohu Basin has undergone a climate and environmental evolution process since Holocene, which is relatively wet → relatively dry→ wet → wet to dry → dry. ③ The variation of weathering intensity also effectively records 9.3, 8.2, 4.2, and 2.8 ka B.P. abrupt events. By combining with the CIA, summer solar insolation since Holocene at 30°N, δ18O records of Sanbao Cave in Shennongjia Mountains, δ13C of Dajiu Lake peat section in Shennongjia Mountains and other comprehensive comparisons since 11 000 cal. a B.P., it is found that the tectonic uplift movement provides stable terrestrial debris material, and the climatic and environmental conditions of the watershed are the controlling factors for the intensity of chemical weathering. The vegetation succession under the background of climate change also affects the strength of weathering, while the particle size mainly affects the chemical element composition of sediment.

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