内蒙古林业科技
內矇古林業科技
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INNER MONGOLIA FORESTRY SCIENCE AND TECHNOLOGY
2012年
2期
36-40
,共5页
苏亚拉%包翔%乌仁苏都%高娃%木其尔
囌亞拉%包翔%烏仁囌都%高娃%木其爾
소아랍%포상%오인소도%고왜%목기이
克鲁伦河%草场利用方式%土壤物理性质
剋魯倫河%草場利用方式%土壤物理性質
극로륜하%초장이용방식%토양물이성질
Kelulun River%grassland utilization pattern%soil physical property
以克鲁伦河下游地区典型草原为研究对象,以传统游牧作为对照,研究探讨了围栏放牧草场利用方式下土壤物理性质变化规律,其研究结果如下:土壤含水量为游牧区〉打草场区〉轮牧区;土壤容重为轮牧区〉打草场〉游牧区;在夏营盘0~10 cm土层中孔隙度的比较结果为:游牧区〉打草场区〉轮牧区。在冬营盘各土层中土壤孔隙度比较结果是,游牧区〉打草场区〉轮牧区。土壤砂粒含量为游牧区〈打草场区〈轮牧区,细粉粒含量游牧区、轮牧与打草场区间均有显著差异,夏营盘和冬营盘的粘粒含量为轮牧区〈打草场区〈游牧区。
以剋魯倫河下遊地區典型草原為研究對象,以傳統遊牧作為對照,研究探討瞭圍欄放牧草場利用方式下土壤物理性質變化規律,其研究結果如下:土壤含水量為遊牧區〉打草場區〉輪牧區;土壤容重為輪牧區〉打草場〉遊牧區;在夏營盤0~10 cm土層中孔隙度的比較結果為:遊牧區〉打草場區〉輪牧區。在鼕營盤各土層中土壤孔隙度比較結果是,遊牧區〉打草場區〉輪牧區。土壤砂粒含量為遊牧區〈打草場區〈輪牧區,細粉粒含量遊牧區、輪牧與打草場區間均有顯著差異,夏營盤和鼕營盤的粘粒含量為輪牧區〈打草場區〈遊牧區。
이극로륜하하유지구전형초원위연구대상,이전통유목작위대조,연구탐토료위란방목초장이용방식하토양물이성질변화규률,기연구결과여하:토양함수량위유목구〉타초장구〉륜목구;토양용중위륜목구〉타초장〉유목구;재하영반0~10 cm토층중공극도적비교결과위:유목구〉타초장구〉륜목구。재동영반각토층중토양공극도비교결과시,유목구〉타초장구〉륜목구。토양사립함량위유목구〈타초장구〈륜목구,세분립함량유목구、륜목여타초장구간균유현저차이,하영반화동영반적점립함량위륜목구〈타초장구〈유목구。
Taking the typical steppe in the downstream region of Kelulun River as the research object and traditional nomadism as control, the changing law of soil physical properties with the grassland utilization pattern of fence grazing has been studied. The results show that the soil water content is nomadic area 〉 clipping pasture area 〉 rotational grazing area, the soil bulk density is rotational grazing area 〉 clipping pasture area 〉 nomadic area. In summer quarter, the soil porosity in 0 - 10 cm layer is nomadic area 〉 clipping pasture area 〉 rotational grazing area. In winter quarter, the soil porosity in each layer is nomadic area 〉 clipping pasture area 〉 rotational grazing area. The soil sand content is nomadic area 〈 clipping pasture area 〈 rotational grazing area. There is obvious difference for fine silt content among nomadic area, clipping pasture area and rotational grazing area. And the clay content in summer quarter and winter quarter is rotational grazing area 〈 clipping pasture area 〈 nomadic area.