干旱区生态环境知识资源中心(Arid): 黄土高原沟壑区草地土壤深层干燥化与氮素消耗

Arid

	黄土高原沟壑区草地土壤深层干燥化与氮素消耗
其他题名	Soil desiccation and nitrogen consumption of artificial meadow in the Loess Plateau
	樊军; 郝明德; 邵明安
来源期刊	自然资源学报
ISSN	1000-3037
出版年	2004
卷号	19 期号:2 页码:201-206
中文摘要	根据设在黄土高原沟壑区旱塬地的长期田间定位试验结合野外调查,对早塬人工草地土壤0～1 000Gm水分含量及剖面氮素含量与分布进行研究.结果显示,旱地人工草地连续种植会显著消耗土壤深层储水与土壤氮素,苜蓿的耗水深度超过1 000cm,剖面200cm以下平均含水量12.6%;同时,也使深层土壤硝态氮含量降低,150cm以下硝态氮含量均小于1mg/kg,荒草地的水分状况好于人工草地,这是因为荒草地的生物量远低于人工草地,200cm以下平均含水量18.8%.在干旱地区,土壤深层储水可以调节植物用水,但是人工苜蓿从土壤深层吸收大量水分导致土壤干燥化的发生.因此,土壤储水的调节作用丧失,合理的草地产量是控制土壤干燥化的途径.草地施肥并没有显著的增产作用,但可以延缓人工草地的衰退时间.因为草地施肥的效益不明显,生产实践中农民并不施肥.
英文摘要	According to a long term experiment in dry land of the Loess Plateau and field survey of wilderness,we studied the distribution of soil water and nitrogen content in the soil profiles. The results showed that artificial meadow could consume lots of soil water in deep layers of soil, and it also absorbed much of nitrogen.The mean soil water content of 200cm ~1 000cm soil layers was 12.6%, furthermore, the nitrate content of 150cm~l 000 cm soil layers was less than lmg/kg. But soil water content of the wilderness was better than that of artificial meadow; the mean soil moisture was 18.8%.In the arid area,the storage water in deep layers of soil can adjust water utilization of plants,but artificial alfalfa can absorb lots of water from deep layers and lead to soil desiccation.Because of in availability of enough water to adjust effects of arid weather on growth of plants,reasonable yield should be advised to control soil desiccation.Fertilizers application can not contribute to yield of grassland distinctly,but it can maintain output of artificial alfalfa to avoid the yield getting down in the short time.Unfortunately,fertilizers were not used in grassland by farmers,because it is difficult to profit from fertilizers application.
中文关键词	土壤水分 ; 草地 ; 土壤干燥化 ; 硝态氮
英文关键词	soil moisture artificial meadow soil desiccation nitrate
类型	Article
语种	中文
国家	中国
收录类别	CSCD
WOS类目	Agriculture
WOS研究方向	Agriculture
CSCD记录号	CSCD:1566438
资源类型	期刊论文
条目标识符	http://119.78.100.177/qdio/handle/2XILL650/205874
作者单位	樊军, 中科院水土保持所, 黄土高原土壤侵蚀与旱地农业国家重点实验室, 杨凌, 陕西 712100, 中国.; 郝明德, 中科院水土保持所, 黄土高原土壤侵蚀与旱地农业国家重点实验室, 杨凌, 陕西 712100, 中国.; 邵明安, 中科院水土保持所, 黄土高原土壤侵蚀与旱地农业国家重点实验室, 杨凌, 陕西 712100, 中国.
推荐引用方式 GB/T 7714	樊军,郝明德,邵明安. 黄土高原沟壑区草地土壤深层干燥化与氮素消耗[J],2004,19(2):201-206.
APA	樊军,郝明德,&邵明安.(2004).黄土高原沟壑区草地土壤深层干燥化与氮素消耗.自然资源学报,19(2),201-206.
MLA	樊军,et al."黄土高原沟壑区草地土壤深层干燥化与氮素消耗".自然资源学报 19.2(2004):201-206.