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991.
用钛白废酸制备氯化铁和硫酸 总被引:1,自引:1,他引:0
采用溶剂萃取与蒸发浓缩相结合的方法综合利用钛白废酸。实验结果表明:向钛白废酸中加入一定量的盐酸,用磷酸三丁酯(TBP)萃取Fe3 ,得到萃合物为HFeCl4.2TBP;在萃取相比(有机相与水相的体积比)与反萃取相比(水相与有机相的体积比)均为1的条件下,用2.53mol/L的TBP对c(Fe3 )=1.023mol/L、c(HCl)=4.53mol/L的试样进行连续5级逆流萃取与反萃取后,得到纯度高达99.88%、总产率达99.4%的氯化铁;萃余液经一次性蒸发浓缩,可得到质量分数80%以上的硫酸。 相似文献
992.
羟基聚合氯化铝铁溶液的形态转化规律 总被引:51,自引:7,他引:44
采用改进的 Al-Fe-Ferron逐时络合比色法和酸滴定实验研究了典型羟基聚合铝铁(nAl/nFe=9∶1,5∶5)溶液的形态转化 .结果表明 ,羟基聚合铝铁的形态转化主要由 nAl/nFe值、碱化度和熟化等因素决定 ;羟基聚合铝铁的形态转化特征是优势形态之间的转变 ;当nAl/nFe>5∶5,随碱化度的升高 ,[Al+Fe]a和 [Al+Fe]b 2类形态逐渐占优势 ;随nAl/nFe值的减小 ,[Al+Fe]a和 [Al+Fe]c增加 ,而 [Al+Fe]b 减少 .讨论了羟基聚合铝铁的形态转化规律 . 相似文献
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997.
Kenneth D. Schmidt 《Journal of the American Water Resources Association》1973,9(3):598-606
ABSTRACT The Cortaro Area is currently the depository for much of the liquid waste from the City of Tucson. In the past, more than one-half of the sewage effluent was used for crop irrigation. However, since 1970 virtually all of the sewage effluent has been percolated in the normally dry Santa Cruz River channel. Nitrate and chloride contents were monitored monthly in water samples from about 20 large-capacity irrigation wells. Contents and seasonal trends for these constituents were closely related to the disposal of sewage effluent. Water quality problems other than nitrate include total dissolved solids, boron, coliform, and lead. High lead contents in the area appear to be a natural phenomenon and the coliform contents are likely related to poor well construction. The other quality problems are primarily due to sewage effluent. 相似文献
998.
ABSTRACT Mass budgets for chloride were estimated from 1975-1978 for the Mississippi River from headwaters to near the mouth to determine the magnitudes of natural and anthropogenic sources. Annual chloride input from precipitation ranged from about 200 kg mi-2yr-1 at Royalton, Minnesota, to about 350 kg mi-2yr-1 at Vicksburg, Mississippi. Mass export ranged from about 900 kg mi-2yr-1 at Royalton to about 8000 kg mi-2yr-1 at Vicksburg. As much as 80 percent of the residual, the difference between input and export, probably is contributed by anthropogenic sources. In particular, semi-logarithmic scatterplots of monthly total discharge against chloride concentration show that, during early spring, chloride elevations in the Mississippi River and Ohio River are elevated, possibly because of flushing of road salt and leaching of chloride from the accumulated snowpack. 相似文献
999.
Jody N. Connor Thomas V. Belanger 《Journal of the American Water Resources Association》1981,17(5):799-805
Direct ground water seepage measurements were made in Lake Washington, Florida, to determine the importance of seepage as a water and chloride source to the lake and upper St. Johns River. Over 200 seepage measurements were made in the lake and adjoining canals from July through December 1978. Results indicated that seepage into the shore areas of Lake Washington was an insignificant water source to the lake, representing 0.6 percent of the inputs, and was nearly balanced by ground water recharge in the midlake region. Drainage canals entering Lake Washington, however, exhibited high average seepage rates (17.7 L/m2-day), over eight times the lake average (2.01 L/M2-day). Discharge from the St. Johns River was the dominant factor in the water budget of Lake Washington and represented approximately 88 percent of the inputs during the study year. Although inputs from the drainage canals represented only 6.6 percent of the St. Johns River annual discharge, these canals represented 20.4 percent of the annual St. Johns River chloride loading and 62.1 percent of the river chloride loading during the five driest months of 1978. Evidence from this study indicates that rising levels of chloride in the river in recent years are largely attributable to ground water seepage in channelized areas, particularly in the headwaters. These chloride inputs assume greater importance during low water/low flow periods. 相似文献
1000.
溴酸钾氧化氨基黑10B催化光度法测定痕量亚硝酸根 总被引:4,自引:0,他引:4
研究了在磷酸介质中 ,痕量亚硝酸根对溴酸钾氧化氨基黑 1 0 B的催化褪色作用 ,建立了催化动力学光度法测定痕量亚硝酸根的新方法 ,并探讨了动力学反应条件 ,方法的线性范围为 0~ 1μg/1 0 ml,检出限为 4.88× 1 0 - 9g/ml,用于地面水及雨水中亚硝酸根的测定 ,结果满意。 相似文献