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Spatial Distribution and Fluorescence Properties of Soil Dissolved Organic Carbon Across a Riparian Buffer Wetland in Chongming Island,China

Spatial Distribution and Fluorescence Properties of Soil Dissolved Organic Carbon Across a Riparian Buffer Wetland in Chongming Island,China

作     者:WANG Yu-Lai YANG Chang-Ming ZOU Li-Min CUI Heng-Zhao 

作者机构:Key Laboratory of Yangtze River Water Environment of the Ministry of EducationTongji University School of Energy and EnvironmentAnhui University of Technology Water Supply Management Station of Shanghai Qingpu Water Authority 

出 版 物:《Pedosphere》 (土壤圈(英文版))

年 卷 期:2015年第25卷第2期

页      面:220-229页

核心收录:

学科分类:09[农学] 0903[农学-农业资源与环境] 090301[农学-土壤学] 

基  金:supported by the Major Science and Technology Program for Water Pollution Control and Treatment of China(Nos.2011ZX07303-001 and 2014ZX07303-003) the State Key Laboratory of Soil and Sustainable Agriculture,Institute of Soil Science,Chinese Academy of Sciences(No.Y412201426) 

主  题:excitation-emission matrix(EEM) riparian buffer zone fluorescence index(FI) humification index(HIX) optical indices 

摘      要:The migration of soil dissolved organic carbon(DOC) from terrestrial to aquatic environments has important impacts on the adjacent water quality and the transport of organic and inorganic ***,few studies have investigated the sources and properties of DOC in riparian zones.A total of 34 soil samples were collected across four riparian buffer zones(Zones A-D) on Chongming Island,*** vertical distributions of soil organic carbon(SOC) and DOC,fluorescence excitation-emission matrix(EEM) spectra of DOC and the optical indices,including fluorescence index(FI),index of recent autochthonous contribution(BIX),and humification index(HIX),were measured across the riparian environment to investigate the sources and fluorescence properties of *** results showed that SOC stored in the surface soil(0-30 cm) accounted for 40%of the total soil profile *** DOC accumulated in Zones A-C,which accounted for 5%of the *** fluorescence EEM spectra of DOC showed that DOC contained humic-like and protein-like substances,which were mainly derived from recent plant debris by microbes.A large amount of humic-like substances were sorbed to minerals in the surface soil(0-30 cm).In addition,the riparian topography and soil physico-chemical properties(pH,EC and moisture) dictated the transformation and transport of *** results suggested that EEMs could reveal the source of DOC in riparian soil systems,and that optical indices were complementary tools that revealed the characteristics of soil DOC and provided supplemental evidence about DOC sources.

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