不同颗粒级配黄土比表面积的预测
Estimation of soil specific surface area of different distribution
土的比表面积是土颗粒表面水分子和离子相互作用的重要参数,土的很多物理和化学性质都和它的比表面积有关,但是比表面积的测量是个耗时和耗力的过程,所以我们可以采用几种不同的方法对土的比表面积进行合理的预测,本文采用了多元线性回归方程和幂函数方程分析得到的两种经验模型和非塑性土模型对Q2黄土、Q3天水马兰黄土、Q3九州台马兰黄土及砂土进行了比表面积预测,结果表明两种经验模型在黄土的比表面积预测中均有较好的效果,幂函数模型整体上优于多元线性回归模型,非塑性土模型只适用于砂土的比表面积预测,不适用于黄土的比表面积预测。
he specific surface of soil (SSA) is crucial for the interaction of ions and water molecules with the soil particles. Therefore, many physical and chemical properties of soil are determined by its specific surface. Because measurement of the specific surface area is a relatively time-consuming and labor-intensive process, So we can use several different methods of soil surface area for a reasonable prediction. In this paper, a multiple linear regression equation and the power function analysis of two kinds of empirical model and non-plastic soils model are used to predict specific surface area of Q2 loess、Q3 Tianshui Malan loess、Q3Jiuzhoutai Malan loess and sand. It is shown that both the Power function model and Multiple linear regression model perform well in predicting specific surface area of the soils, but the former is better in overall performance than the latter, Non-plastic soil model is not applicable for the specific surface area of soils.
张帆宇、谌文武、孙美玲
地质学
比表面积多元线性回归模型幂函数模型非塑性土模型
specific surface areaMultiple linear regression modelPower function modelnon-plastic soils model
张帆宇,谌文武,孙美玲.不同颗粒级配黄土比表面积的预测[EB/OL].(2014-03-20)[2025-08-16].http://www.paper.edu.cn/releasepaper/content/201403-621.点此复制
评论