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水滑石对水溶液中硼的吸附及其在地热除硼中的初步应用。

Boron sorption from aqueous solution by hydrotalcite and its preliminary application in geothermal water deboronation.

机构信息

State Key Laboratory of Biogeology and Environmental Geology & School of Environmental Studies, China University of Geosciences, 430074, Wuhan, Hubei, People's Republic of China,

出版信息

Environ Sci Pollut Res Int. 2013 Nov;20(11):8210-9. doi: 10.1007/s11356-013-1796-5. Epub 2013 May 22.

Abstract

Hydrotalcite and its calcination product were used to treat pure water spiked with various concentrations of boron and geothermal water containing boron as a major undesirable element. The kinetics process of boron sorption by uncalcined hydrotalcite is controlled by the diffusion of boron from bulk solution to sorbent-solution boundary film and its exchange with interlayer chloride of hydrotalcite, whereas the removal rate of boron by calcined hydrotalcite rests with the restoration process of its layered structure. The results of isotherm sorption experiments reveal that calcined hydrotalcite generally has much stronger ability to lower solution boron concentration than uncalcined hydrotalcite. The combination of adsorption of boron on the residue of MgO-Al2O3 solid solution and intercalation of boron into the reconstructed hydrotalcite structure due to "structural memory effect" is the basic mechanism based on which the greater boron removal by calcined hydrotalcite was achieved. As 15 geothermal water samples were used to test the deboronation ability of calcined hydrotalcite at 65 °C, much lower boron removal efficiencies were observed. The competitive sorption of the other anions in geothermal water, such as HCO3-, SO4(2-), and F-, is the reason why calcined hydrotalcite could not remove boron from geothermal water as effectively as from pure boron solution. However, boron removal percents ranging from 89.3 to 99.0% could be obtained if 50 times of sorbent were added to the geothermal water samples. Calcined hydrotalcite is a good candidate for deboronation of geothermal water.

摘要

水滑石及其煅烧产物被用于处理含有硼作为主要不利元素的地热水和各种浓度硼的纯水。未煅烧水滑石吸附硼的动力学过程受硼从主体溶液扩散到吸附剂-溶液边界膜以及与水滑石层间氯化物交换的控制,而煅烧水滑石去除硼的速率取决于其层状结构的恢复过程。等温吸附实验结果表明,煅烧水滑石通常比未煅烧水滑石具有更强的降低溶液硼浓度的能力。硼在 MgO-Al2O3 固溶体残余物上的吸附以及由于“结构记忆效应”而将硼嵌入重建的水滑石结构中,是煅烧水滑石去除硼能力增强的基本机制。当使用 15 个地热水样在 65°C 下测试煅烧水滑石的除硼能力时,观察到去除效率较低。地热水中其他阴离子(如 HCO3-、SO4(2-)和 F-)的竞争吸附是煅烧水滑石不能像从纯硼溶液那样有效地从地热水中去除硼的原因。然而,如果向地热水样品中添加 50 倍的吸附剂,则可以获得 89.3%至 99.0%的硼去除率。煅烧水滑石是地热水除硼的良好候选材料。

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