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横跨中国崇明岛河岸湿地缓冲区土壤中溶解性有机碳的空间分布及其荧光特征
引用本文:WANG Yu-Lai,YANG Chang-Ming,ZOU Li-Min,CUI Heng-Zhao. 横跨中国崇明岛河岸湿地缓冲区土壤中溶解性有机碳的空间分布及其荧光特征[J]. 土壤圈, 2015, 25(2): 220-229
作者姓名:WANG Yu-Lai  YANG Chang-Ming  ZOU Li-Min  CUI Heng-Zhao
作者单位:Key Laboratory of Yangtze River Water Environment of the Ministry of Education,Tongji University;School of Energy and Environment,Anhui University of Technology;Water Supply Management Station of Shanghai Qingpu Water Authority
基金项目: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)
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 contaminants.However,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,China.The 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 DOC.The results showed that SOC stored in the surface soil(0-30 cm) accounted for 40%of the total soil profile SOC.The DOC accumulated in Zones A-C,which accounted for 5%of the SOC.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 DOC.The 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.

关 键 词:excitation-emission matrix(EEM)  riparian buffer zone  fluorescence index(FI)  humification index(HIX)  optical indices

Spatial distribution and fluorescence properties of soil dissolved organic carbon across a riparian buffer wetland in Chongming Island, China
WANG Yu-Lai,YANG Chang-Ming,ZOU Li-Min and CUI Heng-Zhao. Spatial distribution and fluorescence properties of soil dissolved organic carbon across a riparian buffer wetland in Chongming Island, China[J]. Pedosphere, 2015, 25(2): 220-229
Authors:WANG Yu-Lai  YANG Chang-Ming  ZOU Li-Min  CUI Heng-Zhao
Affiliation:1Key Laboratory of Yangtze River Water Environment of the Ministry of Education, Tongji University, Shanghai 200092 (China)2School of Energy and Environment, Anhui University of Technology, Maanshan 243002 (China)3Water Supply Management Station of Shanghai Qingpu Water Authority, Shanghai 201700 (China)
Abstract: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 contaminants. However, 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, China. The 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 DOC. The results showed that SOC stored in the surface soil (0--30 cm) accounted for 40% of the total soil profile SOC. The DOC accumulated in Zones A--C, which accounted for 5% of the SOC. 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 DOC. The 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.
Keywords:excitation-emission matrix (EEM)   riparian bu.er zone   fluorescence index (FI)   humification index (HIX)   optical indices
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