山西太岳山好地方典型植被类型土壤理化特征

生态学杂志

山西太岳山好地方典型植被类型土壤理化特征

纪文婧¹,程小琴¹,韩海荣^1*,康峰峰¹,桂志宏²,朱江¹,王甜¹,周文嵩¹,赵敬^1

（¹ 北京林业大学省部共建森林培育与保护教育部重点实验室，北京 100083； ^2山西省太岳山国有林管理局好地方林场， 山西沁源 046505）

出版日期:2016-01-10 发布日期:2016-01-10

Soil physicochemical properties of typical vegetation types in Haodifang, Taiyue Mountain of Shanxi.

JI Wen-jing¹, CHENG Xiao-qin¹, HAN Hai-rong^1*, KANG Feng-feng¹, GUI Zhi-hong², ZHU Jiang¹, WANG Tian¹, ZHOU Wen-song¹, ZHAO Jing^1

(¹Key Laboratory of Ministry of Forest Cultivation and Conservation of Ministry of Education, Beijing Forestry University, Beijing 100083, China; ^2Haodifang Forest Farm of Taiyue Forestry Bureau in Shanxi, Qinyuan 046505, Shanxi, China).

Online:2016-01-10 Published:2016-01-10

摘要/Abstract

摘要： 以山西太岳山好地方林场4种植被类型（草甸、灌丛、华北落叶松人工林、华北落叶松白桦混交林）0～60 cm土层土壤为研究对象，采取野外定点取样和实验室分析的方法，研究不同植被类型土壤理化性质特征。结果表明：土壤容重和pH值随土层深度的增加而增加；土壤含水量随土层深度增加而减小；不同植被类型间，土壤含水量大小排序为华北落叶松-白桦混交林>草甸>华北落叶松人工林>灌丛；容重为灌丛>华北落叶松-白桦混交林>华北落叶松人工林>草甸；pH值变化规律为华北落叶松-白桦混交林>华北落叶松人工林>灌丛>草甸；土壤有机质、全氮含量随土层深度增加而减小，各土层之间差异显著；全磷和全钾含量各土层间差异不显著；不同植被类型间，草甸土壤有机质、全氮、全磷含量都高于其他3种植被类型，灌丛土壤全钾含量高于其他3种植被类型；土壤有机质与全氮呈极显著正相关；容重与含水量、有机质、全氮呈极显著负相关；pH值与有机质、全氮、全磷呈极显著负相关。

关键词: 水文频率, 水文基因, 非一致性, 进化原理, 常规矩

Abstract: Quantifying changes in soil physicochemical properties of forest ecosystems is important for forest regeneration. In this study, four vegetation types including grassland, shrub land, Larix principisrupprechtii Mayr. pure forest, and L. principisrupprechtii and Betula platyphlla Suk. mixed forest were selected as the research object in Haodifang Forest Farm in Taiyue, Shanxi Province. Soil samples were collected at depths of 0-10, 10-20, 20-30, 30-40, 40-50 and 50-60 cm, to analyze their physicochemical properties. The soil bulk density and pH value increased with the increase of soil depth, while the opposite is true for the soil water content. The soil water content decreased in the following order: L. principisrupprechtii and B. platyphlla mixed forest > grassland > L. principisrupprechtii pure forest > shrub land. The soil bulk density decreased in the order of shrub land > L. principisrupprechtii and B. platyphlla mixed forest > L. principisrupprechtii pure forest > grassland. The pH value ranked as L. principisrupprechtii and B. platyphlla mixed forest > L. principisrupprechtii pure forest > shrub land > grassland. The soil organic matter and total nitrogen (TN) presented a decreasing trend with the increase of soil depth and there were significant differences among different soil layers. There were no significant differences of total phosphorus (TP) and total potassium (TK) among different soil layers. Among the four vegetation types, the contents of soil organic matter, TN and TP in grassland were remarkably higher than that in the other three vegetation types. The TK content in shrub land was higher than that in the other three vegetation types. There was a significant positive correlation between TN and soil organic matter. Soil bulk density was negatively correlated with soil water content, organic matter and TN, and pH value was negatively correlated with soil organic matter, TN and TP.

Key words: hydrological frequency., hydrological gene, evolution principle, moment, non-consistency

纪文婧1,程小琴1,韩海荣1*,康峰峰1,桂志宏2,朱江1,王甜1,周文嵩1,赵敬1. 山西太岳山好地方典型植被类型土壤理化特征[J]. 生态学杂志.

JI Wen-jing1, CHENG Xiao-qin1, HAN Hai-rong1*, KANG Feng-feng1, GUI Zhi-hong2, ZHU Jiang1, WANG Tian1, ZHOU Wen-song1, ZHAO Jing1. Soil physicochemical properties of typical vegetation types in Haodifang, Taiyue Mountain of Shanxi.[J]. cje.