中国黑土资源分布格局与动态分析
Pattern and change of black soil resources in china
查看参考文献11篇
|
文摘
|
该文从冻层的角度分析了黑土性状特点与形成过程，揭示了黑土资源的纬向分布与冻层存在的密切关系，根据季节冻结层底面年平均温度和年平均气温关系式，计算出满足黑土形成所必需的与纬度有关的气温条件，从而证明季节冻层决定了黑土纬向的分布。论文从土壤地质学的角度分析了东北黑土资源的经向分布格局，根据黑土的基本性状反演了第四纪黑土成土环境，说明地质历史时期的一系列构造运动造成了东北地区明显的经向地貌差异，进而影响土壤形成的植被条件、母质条件、水文条件以及元素迁移和聚集，从而限定了黑土资源经向分布范围。探讨了黑土资源数量和质量上的变化及其影响因素，强调了人类不合理的土地利用及化肥、农药的污染是土地资源退化的主要原因。 |
|
其他语种文摘
|
Black soil is famous for its high fertility of soil, which is especially important for agricultural development . It is significant to understand pattern and change of black soil for sustainable use of black soil resources . This paper analyses the distribution pattern of black soil resources according to viewpoint of geo-ped-ology and the distribute of seasonal frozen soil layer in the Songnen plain. Firstly, the close relation between the special forming course and the properties of black soil and frozen layer is analyzed, furthermore, according to the relation formula of annual average temperature at seasonal frozen layer bottom and upper earth, the necessary temperature making black soil develop is obtained. The results indicate that black soil is sure to develop on long-term steady or steady seasonal frozen layer, which is a proof that seasonal frozen layer distribution dominates black soil distribution along latitude. Secondly, the landforms characteristics of black soil at geological historical period is researched, which are vital factors for black soil distribution along longitude. The paper also discusses the change of black soil resources' quantity and quality: It indicates that occupying cultivated land and soil erosion are the leading factors of quantity change for black soil resources; the quality change of black soil resources is an integrated result brought about by natural and human activities factors, the former includes seasonal frozen layer moving northward, rainfall eroding soil, and special topography, landforms, etc. , and the latter involves irrational land use and abusing chemical fertilizer and pesticide. Research results show that physical and chemical properties of black soil have been getting deterioration, moreover , severe soil degradation have occurred. |
|
来源
|
资源科学
,2003,25(3):64-68 【核心库】
|
|
关键词
|
黑土资源
;
分布格局
;
季东动层
;
土壤地质学
;
动态变化
|
|
地址
|
中国科学院东北地理与农业生态研究所, 长春, 130012
|
|
语种
|
中文 |
|
文献类型
|
研究性论文 |
|
ISSN
|
1007-7588 |
|
学科
|
环境保护管理 |
|
基金
|
中国科学院知识创新工程重大项目
;
中国科学院知识创新工程重要方向项目
|
|
文献收藏号
|
CSCD:1307728
|
参考文献 共
11
共1页
|
|
1.
全国土壤普查办公室.
中国土壤,1995
|
CSCD被引
32
次
|
|
|
|
|
2.
陈肖柏. 粘性土冻胀预报新模型.
中国科学.B辑,1991(3):296-306
|
CSCD被引
3
次
|
|
|
|
|
3.
周幼吾.
中国冻土,2000
|
CSCD被引
320
次
|
|
|
|
|
4.
黄大庭.
冰川冻土,1986,8(1):29-39
|
CSCD被引
4
次
|
|
|
|
|
5.
陆景冈.
土壤地质学,1997
|
CSCD被引
10
次
|
|
|
|
|
6.
汪佩芳.
中国东北平原第四纪自然环境形成与演化,1990
|
CSCD被引
2
次
|
|
|
|
|
7.
中国科学院林业土壤研究所.
中国东北土壤,1980
|
CSCD被引
41
次
|
|
|
|
|
8.
周幼吾. 我国东北部冻土温度和分布与气候变暖.
冰川冻土,1996,18(增刊):139-147
|
CSCD被引
18
次
|
|
|
|
|
9.
吉林省土壤肥料总站.
吉林土壤,1998
|
CSCD被引
46
次
|
|
|
|
|
10.
廉毅. 吉林省西部荒漠化发展的陆地卫星遥感监测分析.
气象学报,1999,57(6):662-667
|
CSCD被引
19
次
|
|
|
|
|
11.
孙继敏. 中国东北黑土地的荒漠化危机.
第四纪研究,2001,21(1):72-78
|
CSCD被引
27
次
|
|
|
|
|
了解气象卫星更多信息，请访问