山地草甸土

  • 网络mountain meadow soil
山地草甸土山地草甸土
  1. 在pH2.0的模拟酸雨淋溶下,红壤、黄壤、山地草甸土和紫色土中由矿物风化输入的5种阳离子总量分别为2.94、4.33、4.35和6.04(cmolkg)土,显著大于其它酸雨处理。

    At pH 2.0 , the estimated weathering inputs of the total 5 cations in red soil , yellow soil , meadow soil and purplish soil were 2.94 , 4.33 , 4.35 , and 6.04 cmol / kg soil , respectively , which is significantly greater than other treatments .

  2. 半水成土土纲的潮土和山地灌丛草甸土等土类;

    The order of semi-hydromorphic soil contains the great groups of Chao soil and mountain scrubby-meadow soil .

  3. 大围山土壤分布自下而上依次为山地红壤、山地黄壤、山地黄棕壤和山地灌丛草甸土,在海拔1100m以上的山间盆地和凹地间有草甸、沼泽土分布。

    Soil distribution from the foot to the top were : mountain red soil , mountain yellow soil , mountain yellow-brown soil and mountain meadow soil . Above the 1100 m of absolute altitude of the intermountain basin is bog soil .