首页> 外文期刊>土壤圈:英文版 >Fertility Restoration of Red Soils in Low—Hilly Region of Middle Subtropical China
【24h】

Fertility Restoration of Red Soils in Low—Hilly Region of Middle Subtropical China

机译:中亚热带低丘陵区红壤的肥力恢复

获取原文
获取原文并翻译 | 示例
       

摘要

There are about 1.27 million ha of upland red soils derived from Quaternary red clay facing the degradation in the low-hilly region of the middle subtropical China.From the aspects of chemistry,physics and microbiology,the processes of soil fertility restoration in the surface layer(0-20cm) under three types of land use patterns(i.e.citurs orchard,tea garden and upland)in two provinces were studied in this work.Results showed that the reclamation of eroded waste aldn improved most of soil properties.Soil organic matter,total N and P,available P and K,and exchangeable Ca and Mg increased,but soil total K and exchangeable Al decreased Soil pH decreased by 0.5 unit in the pure tea plantation for 20 years.Soil reclamation increased the percentage of soil micreased by 0.5 unit in the pure tea plantation for 20 years.Soil reclamation increased the percentage of soil microaggregates(<0.25mm),especially those with a diameter of 0.02-0.002mm.Soil total porosity increased in the cultivated lands with the increase of soil aeration and capillary porosity,The number of soil microorganisms increased with reclamation caused mainly by the huge increase of the total amout of bacteria,With the cultivation,the eativity of soil urease and acid phosphatase increased.but that of invertase dropped.
机译:中亚热带低丘地区第四纪红黏土面临退化的旱地红壤约127万公顷。从化学,物理和微生物学的角度,研究了表层土壤肥力的恢复过程。在两个省份的三种土地利用类型(即果园,茶园和高地)下(0-20厘米)进行了研究。结果表明,经过侵蚀的废物的复垦并改善了大部分土壤性质。总磷和氮,有效磷和钾以及可交换的钙和镁增加,但土壤总钾和可交换的铝减少,纯茶园20年的土壤pH值降低了0.5个单位。土壤复垦使土壤微生物的百分比增加了0.5在纯茶园中使用了20年的单位面积。土壤开垦增加了土壤微团聚体的比例(<0.25mm),特别是直径在0.02-0.002mm的土壤微团聚体。耕地的土壤总孔隙度增加了随着土壤通气量和毛细孔率的增加,土壤微生物的数量随开垦的增加而增加,这主要是由于细菌总数的大量增加所致。随着耕作,土壤脲酶和酸性磷酸酶的食用率增加,而转化酶的食用率下降。 。

著录项

获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号