| “三江并流区”不同类型土壤腐殖质特性的研究* |
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| 引用本文： | 王晶,何忠俊,王立东,龙兴智,和顺荣,王建忠,洪常青.“三江并流区”不同类型土壤腐殖质特性的研究*[J].云南农业大学学报,2010,25(5):659-664. |
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| 作者姓名： | 王晶 何忠俊 王立东 龙兴智 和顺荣 王建忠 洪常青 |
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| 作者单位： | [1]云南农业大学资源与环境学院,云南昆明650201 [2]云南省丽江市土壤肥料工作站,云南丽江674100 [3]云南省迪庆州土壤肥料工作站,云南香格里拉674400 |
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| 基金项目： | 云南省科技厅自然科学基金项目 |
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| 摘 要： | 为研究各类型土壤的肥力差异，初步分析了紫色土、黄棕壤、高山草甸土、石灰岩土、棕色针叶林土、棕壤、暗棕壤、红壤这8种典型土壤的腐殖质组成和性质。结果表明：仅红壤、黄棕壤的腐殖质含量属中等含量，其余6种均属高含量。腐殖质组成中，均以胡敏素占绝大多数，除暗棕壤和棕色针叶林土外，各土样中富里酸的有机碳的相对数量均大于胡敏酸的有机碳的相对数量。胡敏素含量与腐殖质、有机碳含量呈极显著相关(P＜001)。8种典型土样的腐殖化程度由高到低依次为:棕色针叶林土＞暗棕壤＞棕壤＞紫色土＞石灰岩土＞黄棕壤＞高山草甸土＞红壤。各土样胡敏酸的复杂程度和化学稳定性序列为棕壤＞暗棕壤＞黄棕壤＞紫色土＞红壤＞棕色针叶林土＞高山草甸土＞石灰岩土。各土样中富里酸的缩合度、芳香度和化学稳定性由高到低依次为:石灰岩土＞高山草甸土＞黄棕壤＞紫色土＞棕色针叶林土＞暗棕壤＞棕壤＞红壤。
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| 关 键 词： | 三江并流区 胡敏酸 富里酸 胡敏素 腐殖质 |
Studies on Humus Characteristics from Different Soils in the Three Parallel Rivers Area |
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| WANG Jing,HE Zhong-jun,WANG Li-dong,LONG Xing-zhi,HE Shun-rong,WANG Jian-zhong,HONG Chang-qing.Studies on Humus Characteristics from Different Soils in the Three Parallel Rivers Area[J].Journal of Yunnan Agricultural University,2010,25(5):659-664. |
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| Authors: | WANG Jing HE Zhong-jun WANG Li-dong LONG Xing-zhi HE Shun-rong WANG Jian-zhong HONG Chang-qing |
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| Institution: | 1.College of Resources and Environmental Science, Yunnan Agricultural University, Kunming 650201，China；2.Soil and Fertilizer Station of Lijiang City of Yunnan Province, Lijiang 674100，China；3. Soil and Fertilizer Station of Diqing of Yunnan Province, Diqing 674400，China |
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| Abstract: | In order to study the nutrition of different soils, the composition and nature of humus from the following 8 soils: purple soil, yellow brown soil, mountain meadow soil, limestone soil, brown coniferous forest soil, brown soil, dark brown soil, red soil, were analyzed. The results showed that the contest of humus was medium in red soil and yellow brown soil, those were high in the other 6 soils. Humin was the main composition of humus.Except dark brown soil and brown coniferous forest soil, the relative quantities of the organic carbon in fulvic acid were sour more than those in humic acid. The humin content was significantly correlated with the contents of humus and organic carbon (P<0.01). The rank of humification degree of 8 soils was as follows: brown coniferous forest soil>dark brown soil>brown soil>purple soil>limestone soil> yellow brown soil> alpine meadow soil> red soil. The ranks of complexity and chemical stability of humic acid were as follows: brown soil> dark brown soil> yellow brown soil> purple soil> red soil> brown coniferous forest soil> alpine meadow soil> limestone soil. The ranks of the condensation degree, aromaticity and chemical stability of fulvic acid were as follows: limestone soil> alpine meadow soil> yellow brown soil> purple soil> brown coniferous forest soil> dark brown soil> brown soil> red soil. |
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| Keywords: | three parallel rivers area humic acid fulvic acid humin humus |
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