IMHE OpenIR  > 山地表生过程与生态调控重点实验室
Rapid weathering processes of a 120-year-old chronosequence in the Hailuogou Glacier foreland, Mt. Gongga, SW China
Zhou, Jun1; Bing, Haijian1; Wu, Yanhong1; Yang, Zijiang1; Wang, Jipeng1,2; Sun, Hongyang1; Luo, Ji1; Liang, Jianhong1,2
Corresponding AuthorWu, Yanhong
2016
Source PublicationGEODERMA
ISSN0016-7061
EISSN1872-6259
Volume267Pages:78-91
SubtypeArticle
AbstractIncreasing numbers of 'young' soil chronosequences have become exposed in global alpine areas as glaciers have retreated due to climate warming since the Industrial Revolution. However, knowledge on the initial stages of weathering at the decadal time scale is limited. Our aim is to reveal the weathering processes and influential factors in a 120-year-old chronosequence on Mt. Gongga in southwest China. Sixty-nine soil samples and 17 water samples were collected from 6 sites with different exposure ages (0, 30, 40, 52, 80 and 120 years). Mineral compositions were determined using X-ray diffractometry, and four mineral pools, i.e., (1) exchangeable cations, (2) carbonates and apatite, (3) biotite and hornblende and (4) refractory minerals, were separated using a sequential extraction method. The results reveal that the soil particle sizes of <2 mu m (clay) in the A horizons increased and the particle sizes of 20 - 2000 mu m (sand) decreased significantly with time. The soil organic carbon accumulation rate was up to 14 g/m(2).yr, which is relatively high compared with other chronosequences of similar age. The weathering can be generally divided into two stages: the first stage was dominated by the weathering of carbonates and was present at sites with an exposure age of <= 52 years; the second stage was characterized by the intense weathering of biotite, hornblende and apatite and was present at the 80- and 120-year old sites, where coniferous trees were the dominant plants. The rapid weathering was a result of the interactions of the lithology, rapid vegetation succession and climate in the Hailuogou Chronosequence. Fine silt was produced in large quantities by the strong glacial abrasion and freeze-thaw cycles, providing rich materials for the subsequent chemical and biogeochemical weathering. The decarbonation and the rapid establishment of the conifer forest due to relatively high temperatures and precipitation promote mineral weathering by decreasing soil pH from 8.5 (0 years) to 4.8 (120 years). The high permeability of the soil horizons due to the high content of rock fragments and abundant precipitation allows water and organic acids to infiltrate and dissolve mineral soils above the impervious bedrock. This study highlights the importance of carbonate weathering in alpine biogeochemical cycling during the initial stage of weathering in granitoid rock areas. Furthermore, our results indicate that the weathering intensity increases with exposure age due to vegetation succession in the early stages of weathering. (c) 2015 Elsevier B.V. All rights reserved.
KeywordMineral Weathering Proglacial Area Water Chemistry Soil Formation Young Chronosequence
Subject Area生物地球化学 ; 自然地理学 ; 土壤物理学 ; 土壤化学
WOS HeadingsScience & Technology ; Life Sciences & Biomedicine
DOI10.1016/j.geoderma.2015.12.024
URL查看原文
WOS Subject ExtendedAgriculture
Indexed BySCI
WOS KeywordINITIAL SOIL DEVELOPMENT ; NOMARSKI DIC MICROSCOPY ; PHOSPHORUS SPECIATION ; DISSEMINATED CALCITE ; DAMMA GLACIER ; RATES ; EVOLUTION ; MOUNTAIN ; ENVIRONMENTS ; SWITZERLAND
Language英语
Quartile2区
TOP
WOS SubjectSoil Science
WOS IDWOS:000369473100010
Funding OrganizationNational Natural Science Foundation of China(41401253 ; Chinese Academy of Sciences(KZZD-EW-TZ-06) ; 41272200)
Citation statistics
Cited Times:20[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.imde.ac.cn/handle/131551/13941
Collection山地表生过程与生态调控重点实验室
Affiliation1.Chinese Acad Sci, Inst Mt Hazards & Environm, Key Lab Mt Surface Proc & Ecol Regulat, Chengdu 610041, Peoples R China
2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
First Author Affilication中国科学院水利部成都山地灾害与环境研究所
Recommended Citation
GB/T 7714
Zhou, Jun,Bing, Haijian,Wu, Yanhong,et al. Rapid weathering processes of a 120-year-old chronosequence in the Hailuogou Glacier foreland, Mt. Gongga, SW China[J]. GEODERMA,2016,267:78-91.
APA Zhou, Jun.,Bing, Haijian.,Wu, Yanhong.,Yang, Zijiang.,Wang, Jipeng.,...&Liang, Jianhong.(2016).Rapid weathering processes of a 120-year-old chronosequence in the Hailuogou Glacier foreland, Mt. Gongga, SW China.GEODERMA,267,78-91.
MLA Zhou, Jun,et al."Rapid weathering processes of a 120-year-old chronosequence in the Hailuogou Glacier foreland, Mt. Gongga, SW China".GEODERMA 267(2016):78-91.
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