碱溶对硅藻土保水渗透性能影响研究

Effect of alkali dissolution on the water retention and permeability of diatomite

  • 摘要: 土壤孔隙结构是影响土壤保水渗透性能的重要因素。硅藻土的多孔特性可以用于土壤保水渗透性能调控,但目前缺乏硅藻土多孔界面特性对保水渗透性能影响的相关研究,且硅藻土的保水渗透性能也未见系统研究。碱溶可以调控硅藻土孔道界面特性。为完善硅藻土调控土壤渗透保水性能应用基础研究,以临江硅藻土为原料,在不同碱溶温度条件下制备碱溶硅藻土,运用SEM、氮气吸附法、FITR表征硅藻土及碱溶硅藻土微观形貌、孔结构、表面官能团,并通过硅藻土渗透率测定、活性炭水容量测定量化硅藻保水渗透性能。结果表明:硅藻土保水渗透性能受硅藻土孔结构和表面性质影响,硅藻土比表面积随碱溶温度升高而增加,使其表面羟基发生变化,导致硅藻土渗透率、水容量随碱溶温度升高而增加。在硅藻土用量50 g、NaOH用量10 g、超纯水用量200 mL、碱溶温度90 ℃、碱溶时间30 min条件下,硅藻土碱溶效果最好,硅藻土渗透率为0.1507 darcy,是未处理硅藻土的14.35倍;硅藻土水容量为290.76%,是未处理硅藻土的1.95倍;硅藻土比表面积由6.487 m2/g提高到9.904m2/g。

     

    Abstract: The pore structure of the soil is an important factor affecting soil water retention and infiltration properties. Diatomite with porous character can be used to regulate the water retention and infiltration performance of soil, however, the research on the influence of pore structure and surface property of diatomite is not enough, and the water retention and infiltration performance of diatomite have not been studied systematically. Alkali dissolution can regulate the pore structure and surface property of diatomite. In order to improve the basic research on the application of diatomite to regulate soil water retention and infiltration performance, Linjiang diatomite was used as the raw material to prepare alkali dissolution diatomite under different alkali dissolution temperatures, which based on the principle that diatomite's main ingredient is amorphous SiO2, and the amorphous SiO2 can react with strong alkali to form sodium silicate at a certain temperature and can be removed by filtration. The microstructure, pore structure and surface functional groups of Linjiang diatomite and alkali dissolution diatomite were characterized by SEM, the low temperature nitrogen adsorption method and FITR. The water retention and permeability of diatomite were quantified by diatomite permeability measurement method and activated carbon water capacity measurement method. The results show that the water retention and permeability of diatomite are affected by the pore structure and surface properties of diatomite. The specific surface area of diatomite increases with the increase of alkali dissolution temperature, which changes the surface hydroxyl group, resulting in the increase of permeability and water capacity of diatomite with the increase of alkali dissolution temperature. Under the conditions of diatomite dosage 50 g, NaOH dosage 10 g, ultrapure water dosage 200 mL, alkali dissolving temperature 90 °C and alkali dissolution time 30 min, the alkali dissolving effect of diatomite is the best, and the permeability of diatomite reaches 0.1507 darcy, which is 14.35 times that of untreated diatomite. The water capacity of diatomite reaches 290.76 %, which is 1.95 times that of untreated diatomite. The specific surface area of diatomite increases from 6.487 m2/g to 9.904 m2/g.

     

/

返回文章
返回