赤塔tpp-1排土场入渗效应区水中硅迁移形式(热力学评价)

L. Zamana, L. I. Usmanova
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引用次数: 0

摘要

使用HydroGeo 32程序进行热力学计算的结果是,确定了Chita TPP-1水力倾灰场沉降池的水和受其影响区域内由于渗透损失而存在的地下水中溶解硅的可能形式。在Si浓度为2.1 ~ 17.8 mg/L时,程序中可用的形式中,(hsi2o6) 3 -占主导地位,其下的h4sio4和sio2含量低6 ~ 8个数量级。在pH值为7.20时,(si2o5) 2 -和(si2o4) 4 -离子的最小计算浓度为n 10 - 21 mg/L。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
FORMS OF SILICON MIGRATION IN WATERS IN THE ZONE OF INFILTRATION EFFECT OF THE CHITA TPP-1 ASH DUMP (THERMODYNAMIC ASSESSMENT)
: As a result of thermodynamic calculations using the HydroGeo 32 program, the possible forms of the presence of dissolved silicon in the waters of the settling tank of the Chita TPP-1 hydraulic ash dump and groundwater in the zone of its influence due to infiltration losses are determined. At Si concentrations of 2.1–17.8 mg/L, of the avail-able forms in the program, (HSi 2 O 6 ) 3 – is predominant, the contents of H 4 SiO 4 and SiO 2 following it are 6–8 orders of magnitude lower. The minimum calculated concentrations ( n 10 –21 mg/L) were obtained for (Si 2 O 5 ) 2 – and (SiO 4 ) 4– ions at pH 7.20.
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