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中国农学通报 ›› 2018, Vol. 34 ›› Issue (20): 92-95.doi: 10.11924/j.issn.1000-6850.casb17120098

• 资源 环境 生态 土壤 气象 • 上一篇    下一篇

呼伦贝尔市农牧交错区典型土壤剖面理化性状特征分析

张蕾,郑利远,于贺,张锦源,徐欣,周珂,陈一民,焦晓光,隋跃宇   

  1. 黑龙江大学农业资源与环境学院,东北林业大学图书馆,黑龙江大学农业资源与环境学院,中国科学院东北地理与农业生态研究所,黑龙江大学农业资源与环境学院,黑龙江大学农业资源与环境学院,中国科学院东北地理与农业生态研究所,黑龙江大学农业资源与环境学院,中国科学院东北地理与农业生态研究所
  • 收稿日期:2017-12-23 修回日期:2018-06-19 接受日期:2018-02-24 出版日期:2018-07-13 发布日期:2018-07-13
  • 通讯作者: 焦晓光
  • 基金资助:
    国家科技基础性工作专项“我国土系调查与《中国土系志(中西部卷)》编制”(2014FY110200);黑龙江大学创新创业项目“蓝靛果种植地适 宜性的分析”(2017316)。

Soil Physical and Chemical Properties of Typical Soil Profiles in the Agro-pastoral Zone in Hulunbuir

  • Received:2017-12-23 Revised:2018-06-19 Accepted:2018-02-24 Online:2018-07-13 Published:2018-07-13

摘要: 以呼伦贝尔市农牧交错区典型土壤(黑土、黑钙土、暗棕壤、草甸土、栗钙土)为研究对象,对比研究不同土壤剖面发生层次容重、机械组成、有机碳、全氮、全磷等理化特征的分布规律。结果表明:在呼伦贝尔市农牧交错区,典型土壤有机碳、全氮、全磷均表现出随土壤剖面深度的增加而降低的趋势,而土壤容重、pH值的变化出现相反的趋势,且不同利用方式下土壤容重、有机碳、全氮、全磷含量的累积量不同,牧草地土壤>农田土壤。不同土壤类型有机碳:黑钙土>黑土>栗钙土>草甸土>暗棕壤;全氮:黑钙土>黑土>栗钙土>草甸土>暗棕壤;全磷:栗钙土>黑土>暗棕壤>草甸土>黑钙土。在所有典型土壤中,全钾和机械组成在土壤剖面层次上无明显规律。

关键词: 枫杨, 枫杨, 散生木, 优树选择, 回归方程拟合, 综合评分法

Abstract: This study focuses on the typical soils, i.e. mollisol, chernozem, dark brown soil, meadow soil and chestnut soil, in the agro- pastoral zone in Hulunbuir. The authors studied the bulk density, texture, soil organic carbon (SOC), total nitrogen (TN), total phosphorus (TP) and total potassium (TK) in different genetic layers of soil profiles to illuminate the distribution characteristics of soil physical and chemical properties in this region. The results showed that SOC, TN and TP all decreased with the increase of soil depth. However, both bulk density and pH value increased with the increase of soil depth. Soils under different utilization patterns also showed significant differences in the distribution of SOC, TN, TP and bulk density, and their contents in grass field was higher than that in farmland. SOC distribution in different soil profiles showed a trend of chernozem> mollisol> chestnut soil> meadow soil> dark brown soil. TN distribution showed a similar trend with SOC. TP distribution showed a trend of chestnut soil> mollisol> dark brown soil> meadow soil> chernozem. In all profiles, TK and texture did not show obvious rules.