首页> 外文会议>West Virginia Surface Mine Drainage Task Force Symposium >PROPOSED CHANGES TO SOIL TAXONOMY THAT MAY AFFECT MINE SOIL CLASSIFICATION
【24h】

PROPOSED CHANGES TO SOIL TAXONOMY THAT MAY AFFECT MINE SOIL CLASSIFICATION

机译:拟议对土壤分类系统的变化可能影响矿山土壤分类

获取原文

摘要

Mine soils begin developing horizons from natural processes after mining excavation and transportation of spoil ceases. Spoil deposits and altered landforms are easily recognized from a distance but the soils in those landforms seldom contain proof of their origin. Soil Taxonomy provides a few diagnostic horizons and materials and classes for mine soils. Most excavated or transported mine soils are identified in one of two suborders (Arents or Orthents) because they have no currently accepted diagnostic features other than remnant fragments of soil material. Mine soils (excavated and dredged) with sulfuric horizons are classified in "Sulf" Great Groups, although dredged deposits without sulfidic materials may classify in the Fluvents or Psamments suborders. There are no provisions in Soil Taxonomy to identify human transported material (HTM), human-manufactured or -modified materials, or to identify mine soils that contain those materials separately from natural soils such as in landslides. New designations and diagnostic layers and horizons are needed to establish new classes in Soil Taxonomy for HTM such as mine soils. The International Committee for Anthropogenic Soils (ICOMANTH) circulated letters requesting input for changes to describe, map, and manage mine soils. Most respondents would like to identify human-transported material with a special horizon prefix where evidence of mechanical transportation is left behind. Spoils left on the surface after surface mining or dredging presently have little variation in classification above the soil series level. Approximately two dozen soil series are available for identifying mine soils, although some of the series have overlapping properties. Many mine soils deposited following passage of the Surface Mining Control and Reclamation Act of 1977 contain densic materials due to compaction during reclamation, although none of the existing series recognize the densic contact that is the dominant factor in interpreting their use and management. Proposals to revise Soil Taxonomy will be submitted following recommendations from ICOMANTH with the goal of providing classes for mine soils with unique properties.
机译:矿山土壤开始在采矿开挖和腐败运输后从自然过程中发展地平线。弃土沉积物和改变的地形很容易从远处识别,但是那些地貌中的土壤很少包含起源的证据。土壤分类法为矿山土壤提供了一些诊断视野和材料和课程。大多数挖掘或运输的矿山土壤是以两个副机(代理人或陈列)之一鉴定的,因为它们目前没有接受土壤材料的残余碎片以外的诊断特征。矿山土壤(挖掘和疏浚)含硫视野是分类的“Sulf”的群体,尽管没有硫化物材料的疏浚沉积物可以在氟工或Psamments副中进行分类。土壤分类法没有任何规定,以鉴定人类运输的材料(HTM),人制造或制定的材料,或鉴定矿山土壤,这些土壤与山体滑坡中的天然土壤分开含有这些材料。需要新的名称和诊断层和视野,以在土壤中的土壤分类中建立新课程,如矿山土壤。国际人为土壤委员会(ICOMANTH)循环信件,要求输入改变以描述,地图和管理矿山土壤。大多数受访者想用特殊的地平线前缀识别人类运输的材料,其中落后机械运输的证据。表面挖掘或疏浚后留在表面上的破坏目前在土壤系列水平上方的分类几乎没有变化。尽管有些系列具有重叠的属性,但虽然有些部分具有重叠的特性,但大约两次土壤系列可用于识别矿山土壤。许多矿井土壤沉积在1977年表面采矿控制和填海动作中沉积的封装载有密度材料,因为在填海过程中压实,尽管现有系列都不识别密度接触,这是解释其使用和管理的主导因素。修改土壤分类法的建议将在ICOManth的建议下提交,其目的是为矿山土壤提供独特的财产。

著录项

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