摘要
在不同牧压下,测定土壤容重(0~20cm)、硬度(地表和0~20cm)、孔隙度、毛管持水量等与土壤压实作用的有关物理指标。结果表明,供试放牧强度(0~6.67羊/hm2)对土壤容重的影响仅局限于0~10cm,其中以0~5cm最显著。0~10cm土壤容重的数学模型为y=1.236+0.595x-7.764*10-3x2,R=0.978。相同放牧强度(20羊/hm2)不同放牧时期(春牧5月22日~6月1日,夏牧7月15~25日,秋收9月3~13日),对土壤容重的影响表现在夏季放牧对于土壤的压实作用最轻,秋季最重,春季居中。每公顷0~4只羊,土壤硬度随着放牧强度的增加而增大,每公顷4~6.67只羊,土壤硬度随着放牧强度的增加而降低。放牧强度对土壤表面硬度和毛管持水量的影响不显著。
Soil bulk density,surface hardness, 0~ 20cm hardness and capillary capacity were tested in grazing gradient in temperatural zone semi-arid steep. The soil type is dark sandy chestnut. Thc grazing intensity range is from 0 to 6. 67 shecps/ha. The research result showed: (1) It is limited (0~ 10cm)soil bulk density change influenced by grazing intensity. The mathematics model between soil bulk density and grazing intensity is Y . Soil compaction is the light grazing in summer (15~25 .July ) , the heavy grazing in autumn (3~ 13, September ),the middle grazing in spring with same grazing intensity (20 sheeps/ha ). (2) Soil hardness (0~ 20cm )increased with grazing intensity increaes from 0 to 4(sheeps/ha ), while soil hardncss (0~ 20cm)decreased with grazing intensity from 4 to 6. 67 (sheeps/ha ).(3) Soil surface hardness and capillary capacity changes are not notable with grazing intensity. (4) Based research result, author divide grazing range into two stages, grazing intensity from 0 to 4 (sheeps/ha ) is called the resilience stage of able retum,other is called real degeneration stage that grazing intensity is from 4 to 6. 67 sheeps/ha. In first stage,soil and vegetation can be returned under it's returnability,but secend stage,natural return is difficult unless taked some artifical ameliorate measures. (5) Author proposed 4sheeps/ha would be high limite that grazing on the sandy dark chestnut steep.
出处
《草地学报》
CAS
CSCD
1999年第3期217-222,共6页
Acta Agrestia Sinica
基金
"九五"攻关项目!96-016-01-01
中国科学院"九五"特支项目!KZ95T-04
内蒙古草原生态系统定位研究站开放站基金
关键词
温带草原
放牧强度
土壤压实效应
草原退化
Inner Mongolia
Temperatural steppe
Grazing presure
Soil compaction
Grassland degradation