首页 | 本学科首页   官方微博 | 高级检索  
     检索      

人工林土壤有机碳组分的化学结构特征分析
引用本文:柏 松,罗 敏,李 晖,何帅.人工林土壤有机碳组分的化学结构特征分析[J].西南民族大学学报(自然科学版),2017,43(5):474-479.
作者姓名:柏 松  罗 敏  李 晖  何帅
作者单位:西南民族大学化学与环境保护工程学院,西南民族大学期刊社,西南民族大学化学与环境保护工程学院,西南民族大学化学与环境保护工程学院
基金项目:国家自然科学基金(31400419);中央高校基本科研业务费专项资金资助 ( 2016NZYQN14).
摘    要:为揭示人工林土壤有机碳组分的稳定性维持机制,以云南松人工林为研究对象,利用土壤有机碳化学分组方法,结合元素分析和傅里叶变换红外光谱分析等多种研究手段,研究土壤三种稳定有机碳组分化学结构特征的差异.结果表明,云南松人工林地土壤三种有机碳组分(胡敏酸HA、富里酸FA和胡敏素HM)具有相似的化学结构和官能团组成,主要含有酚羟基、少量脂族烃基、羧基、酮型羟基、酰胺基团和少量碳水化合物.但随土壤剖面深度增加,土壤有机碳组分的官能团特征存在差异.剖面深层土壤HA中富含脂肪族基团,至亚表层土壤中HA脂肪族基团含量减少,表层土HA中未显示含有脂肪族基团.研究表明,脂肪族基团与土壤有机碳组分稳定性的维持有密切关系.该结果从官能团结构特征角度为揭示人工林土壤有机碳化学稳定机制提供了科学依据.

关 键 词:土壤有机碳    有机碳稳定性    红外光谱  人工林
收稿时间:2017/7/11 0:00:00
修稿时间:2017/7/11 0:00:00

The chemical composition and structural features of soil organic carbon (SOC) in plantation
BAI Song,LUO Min,LI Hui and HE Shuai.The chemical composition and structural features of soil organic carbon (SOC) in plantation[J].Journal of Southwest University for Nationalities(Natural Science Edition),2017,43(5):474-479.
Authors:BAI Song  LUO Min  LI Hui and HE Shuai
Institution:School of chemistry and environment,Southwest University for Nationalities,Periodical office,Southwest University for Nationalities,School of chemistry and environment,Southwest University for Nationalities,School of chemistry and environment,Southwest University for Nationalities
Abstract:To elucidate the stabilization of soil organic carbon (SOC) in plantation, the chemical composition and structural features of soil organic carbon (SOC) in Pinus yunnanensis plantation were studied, based on chemical fractionation, elemental analysis and FTIR analysis. The results indicated that three organic carbon fractions (HA, FA and HM) in plantation soil has the similar chemical composition and structural features. These three stable carbon fractions consisted mainly of phenolic hydroxyl group, tiny amounts of aliphatic alkyl group, carboxyl group, ketonic type alkyl group, amide group, and small quantities of carbohydrat. The functional groups of soil organic carbon fractions showed increasing trends with increasing soil depth. Specifically, the HA in deeper soils contain a large amount of aliphatic group, but a small amount aliphatic group was found in subsurface soil, and none of these group was found in topsoil. Thus, our results suggest that these susceptible groups is closely related to stabilization of soil organic carbon.
Keywords:soil organic carbon  stabilization of organic carbon  FTIR analysis  plantation
本文献已被 CNKI 等数据库收录!
点击此处可从《西南民族大学学报(自然科学版)》浏览原始摘要信息
点击此处可从《西南民族大学学报(自然科学版)》下载免费的PDF全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号