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Laboratory Investigation on the Disintegration Characteristics of Purple Parent Rocks

机译:紫色母岩崩解特性的室内研究

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The paper focused on the disintegration characteristics of purple parent rocks from the K2m, J3t and J1l, Yunnan Province of Southern China under laboratory conditions. The experiment was designed according to applications of water, heat and hydrothermal interaction during five treatments: wetting-drying (WD), saturation (ST), refrigerationheating (RH), a combination of wet-dry and refrigeration-heating (WDRH), and a combination of saturation and refrigeration-heating (STRH). The results showed that the rank order of the disintegration rates was the following: WDRH>STRH> ST>WD>RH. The disintegration rate was a positively with cycle number of the treatment for J1l and K2m, but a negatively correlation for J3t And the disintegration rate was positively correlation with temperature fluctuations and moisture content. The rank order of contribution of the impact factors to rock's disintegration is following: cycle number> temperature change>moisture content.
机译:本文重点研究了在实验室条件下来自中国南方云南省的K2m,J3t和J11l的紫色母岩的崩解特征。该实验是根据五种处理过程中水,热和水热相互作用的应用而设计的:湿法干燥(WD),饱和度(ST),制冷加热(RH),湿法干燥和制冷加热(WDRH)的组合以及饱和度和制冷加热(STRH)的组合。结果表明,崩解速率的等级顺序为:WDRH> STRH> ST> WD> RH。 J1l和K2m的崩解速率与处理的周期数成正相关,而J3t的崩解速率与处理的周期数成负相关,并且崩解速率与温度波动和水分含量成正相关。影响因素对岩石崩解的贡献等级排序为:循环次数>温度变化>水分。

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