排序方式: 共有20条查询结果,搜索用时 15 毫秒
1.
通过沉淀和溶解两方面的实验数据,应用PHREEQC程序模拟了砷酸钙在不同CO2分压条件下溶解度的变化情况,发现环境中的CO2可使砷酸钙盐在酸度较高(pH大于8.3)的条件下发生不一致溶解,使其溶解度升高;CO2分压越大,砷酸钙盐发生不一致溶解的酸度越低;CO2主要影响3∶2和5∶3的砷酸钙盐,而对4∶2砷酸钙盐的影响较小。这对不同类型砷酸钙盐废物的处置是否应考虑CO2的因素提供了依据。 相似文献
2.
金华市大气降水的化学组成特征及来源解析 总被引:3,自引:3,他引:3
对2004年大气降水样品监测资料的综合分析和研究表明,金华市降水样品pH值的分布范围在3.64~6.76之间,降水的酸雨率为79.3%。SO24-和NO-3是降水中主要的阴离子,分别占降水中阴离子总量的66.1%和21.7%。NH 4和Ca2 是降水中含量最高的阳离子,分别占阴离子总量的56.6%和33.4%。降水中这些离子的浓度水平一般比世界上其它地方高,但大大低于国内的北方地区。由于降水中缺乏足够的中和物质,大约76%的降水酸度被NH 4、Ca2 和K 等碱性成分中和。陆源型离子Ca2 、Mg2 和K 以及海盐性离子Na 和Cl-之间存在明显的相关关系,另外Ca2 和SO24-、Mg2 和SO24-、Mg2 和NO-3以及Mg2 和Cl-之间也可以观察到比较好的相关关系。土壤和海水的富集系数表明,研究区域的Ca2 和K 主要来源于岩石/土壤风化,SO24-和NO-3主要归因于人为活动的影响。 相似文献
3.
Seasonal variations in the chemical characteristics of wet and bulk deposition samples collected in Erzurum were investigated for the period March 2002-January 2003. Major cations (Ca2+, K+, Mg2+) and major anions (SO4(2-),NO3-) were determined in bulk and wet deposition samples; pH was also measured in wet deposition. The average pH of the wet deposition at Erzurum was 6.6 due to extensive neutralization of the acidity. A strong relationship between pH and SO4(2-) concentrations was observed in all seasons; however, only a weak relationship was found between pH and NO3-. On a seasonal basis, the correlation between Ca2+ and SO4(2-) concentrations was stronger in winter than in summer. Seasonal variations of ions were examined in both wet and bulk deposition samples. Although maximum concentrations of anions generally occurred during winter and spring, cation concentrations peaked in summer for both wet and bulk deposition. Results indicated that Ca2+ was the dominant cation and SO4(2-) the dominant anion in all deposition samples at Erzurum. Even though correlations among the crustal ions (calcium, magnesium and potassium) were high, the relationship between anthropogenic ions (sulfate and nitrate) was less clear in bulk deposition. 相似文献
4.
对不锈钢管业生产过程产生的废水采用中和、絮凝方法进行处理。出水可以达到国家污水综合排放标准(GB8978—1996)新建一级标准。利用该工艺处理废水的特点是工艺简单、投资省、占地小、操作简单、运行稳定、处理效果好。 相似文献
5.
味精废水的预处理试验研究 总被引:1,自引:0,他引:1
针对味精废水的“五高二低”问题,对其进行了高速离心分离菌体、加石灰水中和沉淀SO24-、离子交换回收谷氨酸联合处理及絮凝沉降+石灰水中和沉淀处理等方法的试验研究,得出采用上述两种联合预处理后,能大部分去除废水中的SS、NH3-N、SO24-,可以满足后续生化处理的要求。在实际应用中如何选用,需结合经济效益与处理效果进行综合分析。 相似文献
6.
7.
采用“氧化还原+中和反应+高效凝聚”工艺处理废蓄电池回收和电池制造企业生产废水。总处理水量为208m^3/d;进水水质:pH:1-2、总铅:13.5mg/L、SS:450mg/L。经该工艺处理后,废水中的总铅、pH、SS等指标均能达标排放。 相似文献
8.
Biological mine drainage treatment 总被引:1,自引:0,他引:1
Drainage from sulphur mines contains a high concentration of ferrous iron and it is strongly acidic. The mechanism of acid mine drainage formation was briefly explained. As a case study, successful measures taken at the abandoned Matsuo mine, Iwate Prefecture, Japan, for preventing the pollution in receiving rivers was presented in this paper. The measures consisted of the construction works against pollution sources and the construction of a drainage treatment plant in which Thiobacillus ferrooxidans oxidizes ferrous iron under a low pH condition, and produced ferric iron is removed by sedimentation. Then, a laboratory-scale fluidized bed reactor using anion exchange resin as attaching material for the bacteria was examined in order to improve the efficiency of biological oxidation of ferrous iron. More than 90% of oxidation had been maintained for 2 months at 1 h of HRT, which suggests that the size of the oxidation tank could be reduced. 相似文献
9.
Precipitation Chemistry and Occurrence of Acid Rain Over Dhanbad, Coal City of India 总被引:1,自引:0,他引:1
Singh AK Mondal GC Kumar S Singh KK Kamal KP Sinha A 《Environmental monitoring and assessment》2007,125(1-3):99-110
The present study investigated the chemical composition of wet atmospheric precipitation over Dhanbad, coal city of India.
The precipitation samples were collected on event basis for three years (July 2003 to October 2005) at Central Mining Research
Institute. The precipitation samples were analyzed for pH, conductivity, major anions (F, Cl, NO3, SO4) and cations (Ca, Mg, Na, K, NH4). The pH value varied from 4.01 to 6.92 (avg. 5.37) indicating acidic to alkaline nature of rainwater. The pH of the rainwater
was found well above the reference pH (5.6), showing alkalinity during the non-monsoon and early phase of monsoon, but during
the late phase of monsoon, pH tendency was towards acidity (<5.6~pH) indicating the non-availability of proper neutralizer
for acidic ions. The observed acidic events at this site were 91, (n = 162) accounting 56% for the entire monitoring months. The (NO3 + Cl)/SO4 ratio in majority of samples was found below 1.0, indicating that the acidity is greatly influenced by SO4. The calculated ratio of (Ca + NH4)/(NO3 + SO4) ranges between 0.42–5.13 (average 1.14), however in most of the samples, the ratio is greater than unity (>1.0) indicating
that Ca and NH4 play an important role in neutralization of acidic ions in rainwater. Ca and SO4 dominate the bulk ionic deposition and these two ions along with NH4 accounts 63% of the annual ionic deposition. 相似文献
10.
在按降雨天气系统和雨前大气颗粒物不同平衡状念对雨样进行分类的基础上,建立了大气颗粒物对降水酸度缓冲作用的计算公式。实例计算表明,计算酸度与清洁点上实测酸度十分一致;颗粒物所消耗的[H~+]占实测[H~+]的24%,占总缓冲能力的44%。 相似文献