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东部沙区表土有机质和速效养分与风沙环境关系初探
  • ISSN号:1000-6060
  • 期刊名称:《干旱区地理》
  • 时间:0
  • 分类:S153.6[农业科学—土壤学;农业科学—农业基础科学]
  • 作者机构:北京师范大学地表过程与资源生态国家重点实验室,防沙治沙教育部工程研究中心,北京100875
  • 相关基金:国家自然科学基金项目(41330746); 中央高校基本科研业务费专项资金(2012LZD13)
中文摘要:

东部沙区表土有机质、速效养分含量普遍较低。按照库布齐沙漠、毛乌素沙地、浑善达克沙地、科尔沁沙地和呼伦贝尔沙地的次序,有机质和速效K含量逐渐增大,这种分布格局与区域风沙环境性质、风沙活动方式密切相关;各沙漠/沙地内部,表土有机质和速效K含量分别与植被盖度、颗粒平均粒径、分选系数之间存在较好的相关性。速效N和速效P含量未表现出上述变化规律。可见有机质和速效K含量对风沙环境的变化较为敏感,因而其在表土中的再分配可以在一定程度上反映局地风沙环境的变化,而速效N和速效P对风沙环境的指示意义不明显。东部沙区表土有机质、速效N及速效P含量普遍高于西部沙区,而速效K含量明显偏低。

英文摘要:

The main objective of the research is to determine the relationship between soil nutrients distribution of surface sediments and the aeolian environment in the eastern desert regions of China. Sediment samples of sand dunes with different mobility at the five deserts in theses area are collected,including Hobq Desert,Mu Us Sandy Land,Otindag Sandy Land,Horqin Sandy Land and the Hulunbuir Sandy Land. The contents of organic matter and available nutrients were tested. Analysis of their spatial characteristics and the correlation between soil nutrients and mean grain size,sorting coefficient,vegetation coverage,regional wind force and dune activity index shows that contents of organic matter and available nutrients are generally very low for all five deserts. From the west to the east,in the order of Hobq Desert,Mu Us Sandy Land,Otindag Sandy Land,Horqin Sandy Land and Hulunbuir Sandy Land,contents of organic matter and available potassium increase gradually. The low contents of organic matter and nutrients in Hobq Desert are closely associated with aeolian activities characterized by frequently alternated occurrence of wind erosion,particle transportation and deposition. Such an aeolian environment is favorable for particle sorting but unfavorable for accumulation of soil nutrients. In Hulunbuir Sandy Land,precipitation is relatively sufficient and the vegetation coverage and the background of soil nutrients are better than those of the other deserts,the strongest regional wind force results in a wind erosion process that dominates aeolian environment. Therefore,physic-chemical properties of the surface sediments are mainly determined by the regional background with high content of soil nutrients. In Mu Us,Otindag and Horqin Sandy Lands,the interlace distribution of wind erosion dominated areas with sparse vegetation and the aeolian deposition dominated areas with good vegetation cover produce a more complex regional aeolian environment than the Hobq and Hulunbuir Sandy Lands,which reduces the loss of soil nutrient

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期刊信息
  • 《干旱区地理》
  • 北大核心期刊(2011版)
  • 主管单位:中国科学院出版委
  • 主办单位:中国科学院新疆生态与地理研究所 新疆地理学会
  • 主编:陈曦
  • 地址:乌鲁木齐北京南路818号
  • 邮编:830011
  • 邮箱:aridlg@ms.xjb.ac.cn
  • 电话:0991-7885506
  • 国际标准刊号:ISSN:1000-6060
  • 国内统一刊号:ISSN:65-1103/X
  • 邮发代号:58-45
  • 获奖情况:
  • 1994-1996、1997-1999年度科技期刊质量评比优秀期...,1999-2000年度科技期刊质量评比优秀期刊二等奖
  • 国内外数据库收录:
  • 英国农业与生物科学研究中心文摘,日本日本科学技术振兴机构数据库,中国中国科技核心期刊,中国北大核心期刊(2004版),中国北大核心期刊(2008版),中国北大核心期刊(2011版),中国北大核心期刊(2014版),中国北大核心期刊(2000版)
  • 被引量:18207