| 香港土壤研究Ⅱ.土壤硒的含量、分布及其影响因素 |
| |
| 引用本文： | 章海波,骆永明,吴龙华,张甘霖,赵其国,黄铭洪.香港土壤研究Ⅱ.土壤硒的含量、分布及其影响因素[J].土壤学报,2005,42(3):404-410. |
| |
| 作者姓名： | 章海波 骆永明 吴龙华 张甘霖 赵其国 黄铭洪 |
| |
| 作者单位： | 章海波（中国科学院南京土壤研究所与香港浸会大学土壤与环境联合开放研究实验室,土壤与环境生物修复研究中心,土壤与农业可持续发展国家重点实验室,南京,210008;中国科学院研究生院,北京,100039）
骆永明（中国科学院南京土壤研究所与香港浸会大学土壤与环境联合开放研究实验室,土壤与环境生物修复研究中心,土壤与农业可持续发展国家重点实验室,南京,210008;中国科学院研究生院,北京,100039）
吴龙华（中国科学院南京土壤研究所与香港浸会大学土壤与环境联合开放研究实验室,土壤与环境生物修复研究中心,土壤与农业可持续发展国家重点实验室,南京,210008;中国科学院研究生院,北京,100039）
张甘霖（中国科学院南京土壤研究所与香港浸会大学土壤与环境联合开放研究实验室,土壤与环境生物修复研究中心,土壤与农业可持续发展国家重点实验室,南京,210008;中国科学院研究生院,北京,100039）
赵其国（中国科学院南京土壤研究所与香港浸会大学土壤与环境联合开放研究实验室,土壤与环境生物修复研究中心,土壤与农业可持续发展国家重点实验室,南京,210008;中国科学院研究生院,北京,100039）
黄铭洪（香港浸会大学裘搓环境科学研究所,香港九龙塘） |
| |
| 基金项目： | 国家重点基础研究发展规划项目(2002CB410810/09)、中国科学院知识创新工程重要方向项目(KIC×3-SW-429) |
| |
| 摘 要： | 基于香港地区51个剖面土壤和44个表层土壤中总硒量的分析,对香港土壤硒含量、分布及其影响因素进行研究.分析结果表明,香港土壤总硒量变幅在0.07～2.26 mg kg-1,平均含量为0.76 mg kg-1,在湿润铁铝土中的硒含量最高,平均为1.05 mg kg-1,含量最低的为旱耕人为土,平均为0.45 mg kg-1;在土壤剖面中硒主要分布在心土层和底土层.林地土壤硒含量(1.36 mg kg-1)较高, 农业土壤较低(0.36 mg kg-1).影响香港土壤硒含量及其分布的因素主要是成土母质.土壤pH值、有机质、粘粒和Fe、Al的含量也是影响土壤硒富集与分布的因素.
|
| 关 键 词： | 香港土壤 硒 分布 影响因素 |
| 收稿时间： | 6/2/2004 12:00:00 AM |
| 修稿时间： | 2004年6月2日 |
HONG KONG SOIL RESEARCHES Ⅱ. DISTRIBUTION AND CONTENT OF SELENIUM IN SOILS |
| |
| Zhang Haibo,Luo Yongming,Wu Longhu,Zhang Ganling,Zhao Qiguo and Wong Minghung.HONG KONG SOIL RESEARCHES Ⅱ. DISTRIBUTION AND CONTENT OF SELENIUM IN SOILS[J].Acta Pedologica Sinica,2005,42(3):404-410. |
| |
| Authors: | Zhang Haibo Luo Yongming Wu Longhu Zhang Ganling Zhao Qiguo and Wong Minghung |
| |
| Affiliation: | Soil and Environmental Bioremediation Center of Institute of Soil Science, CAS, Soil and Environment Joint Open Laboratory, Key State Laboratory of Soil and Agricultural Sustainable Development, Nanjing 210008, China;Graduate School of the Chinese Academy of Sciences, Beijing 100039, China;Soil and Environmental Bioremediation Center of Institute of Soil Science, CAS, Soil and Environment Joint Open Laboratory, Key State Laboratory of Soil and Agricultural Sustainable Development, Nanjing 210008, China;Graduate School of the Chinese Academy of Sciences, Beijing 100039, China;Soil and Environmental Bioremediation Center of Institute of Soil Science, CAS, Soil and Environment Joint Open Laboratory, Key State Laboratory of Soil and Agricultural Sustainable Development, Nanjing 210008, China;Graduate School of the Chinese Academy of Sciences, Beijing 100039, China;Soil and Environmental Bioremediation Center of Institute of Soil Science, CAS, Soil and Environment Joint Open Laboratory, Key State Laboratory of Soil and Agricultural Sustainable Development, Nanjing 210008, China;Graduate School of the Chinese Academy of Sciences, Beijing 100039, China;Soil and Environmental Bioremediation Center of Institute of Soil Science, CAS, Soil and Environment Joint Open Laboratory, Key State Laboratory of Soil and Agricultural Sustainable Development, Nanjing 210008, China;Graduate School of the Chinese Academy of Sciences, Beijing 100039, China;Croucher Institute for Environmental Science, Hong Kong Baptist University, Kowloon Tong, Hong Kong, China |
| |
| Abstract: | The main objective of this project is to study distribution and concentration of selenium (Se) and its affecting factors in Hong Kong soils.Soil samples were collected from fifty-one soil profiles and 44 surface soil layers at 44 sampling sites throughout Hong Kong for analysis of total Se with the aid of the induct ively coupled plasma spectrophotometry.The results indicate that Se was mainly distributed in B and C horizon.Concentrations of total Se in all the soil samples ranged from 0.07 mg kg-1 to 2.26 mg kg-1 (dry wt.), with the lowest and highest concentrat ions recorded in Orthic Anthrosols (average 0.45 mg kg-1, dry wt.) and Udic Ferralisols (average 1.05 mg kg-1, dry wt.) respectively.In terms of land use, the highest and lowest concentrations were recorded in forest soil (average 1.36 mg kg-1, dry wt.), and agricultural soil (average 0.36 mg kg-1, dry wt.) respect ively.The main factor that influences Se concentration and distribution in Hong Kong soils was the parent material.Other soil factors such as soil pH, organic matter, clay fraction, iron and aluminum also played relatively important roles. |
| |
| Keywords: | Hong Kong soil Selenium (Se) Distribution Influencing factors |
| 本文献已被 万方数据 等数据库收录！ |
| 点击此处可从《土壤学报》浏览原始摘要信息 |
|
点击此处可从《土壤学报》下载全文 |
|
