...
首页> 外文期刊>ペドロジスト >Mineral nutrient distributions in tropical peat soil of Riau, Indonesia with special reference to peat thickness
【24h】

Mineral nutrient distributions in tropical peat soil of Riau, Indonesia with special reference to peat thickness

机译:印度尼西亚廖内热带泥炭土壤中的矿质养分分布,特别涉及泥炭厚度

获取原文
获取原文并翻译 | 示例
   

获取外文期刊封面封底 >>

       

摘要

Parts of the tropical peatland in Indonesia are used for plantations such as oil palm and para rubber. This is despite the fact that the mineral nutrient status of the land has not been clearly shown, which may lead to inefficient production and land abandonment. The objective of the present study was to reveal the distribution of each mineral nutrient, i.e. Ca, Mg, K, P and Fe with special reference to peat thickness. Surface (0-25 cm) and subsurface (25-50 cm) peat samples were taken from 42 points in 40 km~2 of oil palm plantation and two points in adjacent forest. Deeper samples were also taken at eight points along two transects to the depth of the mineral soil surface. The ash content, exchangeable bases, total amounts of minerals, and Truog P were determined. The ash content, exchangeable Ca and Mg and total amounts of Mg, K and Fe had a negative correlation with peat thickness, while exchangeable K and Na, Truog P, total Ca and P did not. Some points with a peat thickness of <3 m had high mineral contents that correlated with peat thickness, i.e. high mineral contents were found at the edge of the peat dome. In the profile, ash content, exchangeable Ca, Mg, K, and Na were high at the surface 0.5 m and at 1-2 m above the mineral soil surface. This distribution in the profile corresponds with the boundary thickness of 3 m which is considered to be the absorption threshold of these elements by plants. Amounts of fertilizer may be modified based on the distribution of each mineral nutrient.
机译:印度尼西亚的热带泥炭地的一部分用于种植,如油棕和橡胶。尽管没有清楚显示土地的矿物质营养状况,但这可能导致生产效率低下和土地被遗弃。本研究的目的是揭示各种矿物质营养素(钙,镁,钾,磷和铁)的分布,并特别参考泥炭厚度。从40 km〜2的油棕种植园中的42个点和相邻森林中的两个点采集了表层(0-25 cm)和地下(25-50 cm)泥炭样品。还沿着两个样点在八个点采集了更深的样品,深度达到了矿物土壤表面的深度。测定了灰分,可交换碱,矿物质总量和TruogP。灰分,可交换的Ca和Mg以及Mg,K和Fe的总量与泥炭厚度呈负相关,而可交换的K和Na,Truog P,总Ca和P则不相关。泥炭厚度<3 m的某些点具有与泥炭厚度相关的高矿物质含量,即在泥炭穹顶边缘发现高矿物质含量。在剖面中,灰分含量,可交换的Ca,Mg,K和Na在矿物土壤表面以上0.5 m和1-2 m处较高。轮廓中的此分布对应于3 m的边界厚度,这被认为是植物对这些元素的吸收阈值。可以根据每种矿质养分的分布来调整肥料的用量。

著录项

  • 来源
    《ペドロジスト》 |2013年第2期|64-71|共8页
  • 作者单位

    Graduate School of Agriculture, Kyoto University, Kyoto 606-8502, Japan,Graduate School of Global Environmental Studies, Kyoto University, Kyoto 606-8501, Japan;

    Graduate School of Agriculture, Kyoto University, Kyoto 606-8502, Japan;

    Faculty of Education and Teacher Training, University of Riau, Riau, Indonesia;

    Faculty of Agriculture, Bogor Agricultural University, Bogor 16680, Indonesia;

    Graduate School of Agriculture, Kyoto University, Kyoto 606-8502, Japan,Graduate School of Global Environmental Studies, Kyoto University, Kyoto 606-8501, Japan;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    peat thickness; peat dome; ash content; exchangeable bases;

    机译:泥炭厚度泥炭圆顶灰分;可互换的基础;

相似文献

  • 外文文献
  • 中文文献
  • 专利
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