Effect of Temperature, pH and Salt on Fluorescent Quality of Water Extractable Organic Matter in Black Soil

Water erosion is the major reason for the loss of soil organic carbon in the Northeast China, which leads to the soil quality deterioration and adjacent water pollution. In this study, the effect of extraction temperature, pH value, and salt on the water extractable organic matter (WEOM) was determi...

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Main Authors: Ming-tang LI, Lan-po ZHAO, Jin-jing ZHANG
Format: Article
Language:English
Published: Elsevier 2013-07-01
Series:Journal of Integrative Agriculture
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S2095311913604360
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spelling doaj-1dbe463b4c0a4abdac154f80b49c04d42021-06-07T06:48:57ZengElsevierJournal of Integrative Agriculture2095-31192013-07-0112712511257Effect of Temperature, pH and Salt on Fluorescent Quality of Water Extractable Organic Matter in Black SoilMing-tang LI0Lan-po ZHAO1Jin-jing ZHANG2College of Resource and Environmental Science, Jilin Agricultural University, Changchun 130118, P.R. ChinaZHAO Lan-po, Tel: +86-431-84532955; College of Resource and Environmental Science, Jilin Agricultural University, Changchun 130118, P.R. ChinaCorrespondence ZHANG Jin-jing, Tel: +86-431-84532955; College of Resource and Environmental Science, Jilin Agricultural University, Changchun 130118, P.R. ChinaWater erosion is the major reason for the loss of soil organic carbon in the Northeast China, which leads to the soil quality deterioration and adjacent water pollution. In this study, the effect of extraction temperature, pH value, and salt on the water extractable organic matter (WEOM) was determined by means of the UV absorbance, fluorescence excitation-emission matrix, and derived fluorescence indexes. In general, the carbon content and aromaticity of WEOM increased with the increasing of extraction temperature, with the exception that there was no significant difference in the amount at 0 and 20°C. More fluorophores, especially microbially-derived organic matter were extracted at high temperature. The pH values of extractant, including 5, 7, and 10, showed no effect on the carbon amount of WEOM, whereas the aromaticity and microbially-derived component gradually increased with the increasing of pH values. The fluorescence intensity of humic acid-like fluorophore was stronger in neutral and alkali condition than that in acidic condition. The addition of 10 mmol L−1 CaCl2 significantly decreased the carbon amount of recovered WEOM. Moreover, it significantly decreased the aromaticity of WEOM and the quantity of fulvic acid-like and humic acid-like fluorophores, whereas increased the percentage of tyrosine-like and tryptophan-like fluorophores in the total fluorophores and the amount of microbially-derived organic matter. Generally, 10 mmol L−1 KCl showed the same influence trend, but with low influence degree.http://www.sciencedirect.com/science/article/pii/S2095311913604360black soilwater extractable organic mattersoil profilefluorescence spectroscopy
collection DOAJ
language English
format Article
sources DOAJ
author Ming-tang LI
Lan-po ZHAO
Jin-jing ZHANG
spellingShingle Ming-tang LI
Lan-po ZHAO
Jin-jing ZHANG
Effect of Temperature, pH and Salt on Fluorescent Quality of Water Extractable Organic Matter in Black Soil
Journal of Integrative Agriculture
black soil
water extractable organic matter
soil profile
fluorescence spectroscopy
author_facet Ming-tang LI
Lan-po ZHAO
Jin-jing ZHANG
author_sort Ming-tang LI
title Effect of Temperature, pH and Salt on Fluorescent Quality of Water Extractable Organic Matter in Black Soil
title_short Effect of Temperature, pH and Salt on Fluorescent Quality of Water Extractable Organic Matter in Black Soil
title_full Effect of Temperature, pH and Salt on Fluorescent Quality of Water Extractable Organic Matter in Black Soil
title_fullStr Effect of Temperature, pH and Salt on Fluorescent Quality of Water Extractable Organic Matter in Black Soil
title_full_unstemmed Effect of Temperature, pH and Salt on Fluorescent Quality of Water Extractable Organic Matter in Black Soil
title_sort effect of temperature, ph and salt on fluorescent quality of water extractable organic matter in black soil
publisher Elsevier
series Journal of Integrative Agriculture
issn 2095-3119
publishDate 2013-07-01
description Water erosion is the major reason for the loss of soil organic carbon in the Northeast China, which leads to the soil quality deterioration and adjacent water pollution. In this study, the effect of extraction temperature, pH value, and salt on the water extractable organic matter (WEOM) was determined by means of the UV absorbance, fluorescence excitation-emission matrix, and derived fluorescence indexes. In general, the carbon content and aromaticity of WEOM increased with the increasing of extraction temperature, with the exception that there was no significant difference in the amount at 0 and 20°C. More fluorophores, especially microbially-derived organic matter were extracted at high temperature. The pH values of extractant, including 5, 7, and 10, showed no effect on the carbon amount of WEOM, whereas the aromaticity and microbially-derived component gradually increased with the increasing of pH values. The fluorescence intensity of humic acid-like fluorophore was stronger in neutral and alkali condition than that in acidic condition. The addition of 10 mmol L−1 CaCl2 significantly decreased the carbon amount of recovered WEOM. Moreover, it significantly decreased the aromaticity of WEOM and the quantity of fulvic acid-like and humic acid-like fluorophores, whereas increased the percentage of tyrosine-like and tryptophan-like fluorophores in the total fluorophores and the amount of microbially-derived organic matter. Generally, 10 mmol L−1 KCl showed the same influence trend, but with low influence degree.
topic black soil
water extractable organic matter
soil profile
fluorescence spectroscopy
url http://www.sciencedirect.com/science/article/pii/S2095311913604360
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