首页> 外文会议>International Mine Water Association Symposium >Use of teoslometers to determine the Moisture Characterization Point in ores
【24h】

Use of teoslometers to determine the Moisture Characterization Point in ores

机译:使用Teoslometers以确定矿石中的水分表征点

获取原文

摘要

The Moisture Characterization Point (MCP) of an ore is based on the moisture behavior in the unsaturated pores, close to but below the field capacity of the ore. The MCP is an alternative method to determine safe moisture limits for the shipment of ore as compared to geotechnical test methods used to determine the Transportable Moisture Limit (TML) in ores, such as the Proctor Fagerberg test.In this study a soil tensiometer (Hensley 2009) was adapted to measure the suction pressure (pF) as function of the moisture content in the ore. The Moisture Characterization Point (MCP) was defined as a suction pressure of-0,25 bar. This point is below, but relative close to, the field capacity of the ore. The MCP was correlated with the physical and chemical properties of the ores, like particle size, specific surface area and mineral composition of the ores.The results showed a wide variation in the MCP's for nine different ores, varying between a MCP moisture content of 3.8% up to 21.5 %. The results where compared with the TML limit based on the Proctor Fagerberg tests. For most ores the MCP and TML levels are close (on average a relative difference of 10% between the TML and MCP). For ores with a substantially larger difference then 10%o, the ores mineralogy is a dominant factor. The ore mineralogy could be linked to the ore surface area, leading to the conclusion that shipment of ore with goethite content above 35%> is not liable to liquefy.A better understanding of the moisture behavior in ores has assisted in the development of safer cargo schedules (HVIO 2013) to ensure the safe shipping of bulk cargoes.
机译:矿石的湿度表征点(MCP)基于不饱和孔中的水分行为,接近但低于矿石的场路能力。 MCP是一种替代方法,用于确定与用于确定矿石中的可运输水分极限(TML)的岩土测试方法相比,以确定矿石的安全性水分限制,例如Proctor Fagerberg测试。本研究了土壤张力计(Hensley 2009年)适于测量吸入压力(PF)作为矿石中水分含量的作用。水分表征点(MCP)定义为0,25巴的吸入压力。这一点低于,但相对接近,矿石的现场容量。 MCP与矿石的物理和化学性质相关,如粒径,比表面积和矿物质的矿物成分。结果表明MCP的九种不同矿石的宽变化,在3.8的MCP水分含量之间变化。 %达21.5%。结果与基于Proctor Fagerberg测试的TML限制相比。对于大多数ORES,MCP和TML级别关闭(平均TML和MCP之间的相对差异为10%)。对于具有基本上更大的差异而差异,10%O,矿物学是一种显性因素。矿石矿物学可能与矿石表面积相关联,导致矿石在35%以上的矿石含量发货并不倾向于液化。更好地了解矿石中的水分行为有助于发展更安全的货物计划(2013年HVIO),以确保散货的安全运输。

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