电石渣在煤泥水混凝中的作用机理研究

电石渣在煤泥水混凝中的作用机理 :电石渣对煤泥水混凝作用不是补给了 OH- ,而是提供了大量的 Ca2 + 。Ca2 +通过压缩双电层 ,破坏了煤泥颗粒的稳定性 ,从而使煤泥颗粒发生凝聚。OH-和 Ca( OH) 2 对煤泥水的混凝不直接起作用。     

碳酸锶废水对生态环境的影响调查及治理方案

碳酸锶因电子工业飞速发展而身价百倍，但其生产废水的直接排放则造成了严重的环境污染，本文通过对水体、农业、渔业、人体健康和水生生物等多种因素调查，掌握了碳酸锶废水污染成因，同时提出了资源再利用方案。     

Application of lime and calcium hypochlorite in the dephenolisation and discolouration of olive mill wastewater

The application of hypochlorite for the removal of soluble COD, phenolic and polyphenolic like compounds, and other organic compounds responsible for the olive mill wastewater (OOWW) colour has been experimentally studied. After the OOWW filtration on a sand column, the effluent was subjected to a fast liming under optimal conditions. Lime application reduced polyphenols, COD and SS contents to half of their initial values but an important blackening of the treated OOWW was observed, especially when adding high concentrations of lime (10% (W/V) and 15% (W/V)).A second stage of treatment was applied using calcium hypochlorite. In this stage, removal of the studied compounds reached as much as 95% at higher concentrations, and particularly the colouring of OOWW which is generally difficult to eliminate was greatly reduced. The OOWW hypochloration acted through coagulation–flocculation and a rapid oxidation of the organic matter proceeded from the first 5 min. The kinetic study of the degradation of the waste polluting compounds from liming showed that Ca(ClO)₂ reacts similarly in the elimination of organic compounds, polyphenols, SS and colouration. The analysis of the organochloride compounds generated by the reaction between hypochlorite and the organic compounds showed that DDD, DDT and the heptachlor contents exceeded the values recommended by the International and European drinking water standards.     

碳酸钙改性硅藻土处理电解锌漂洗废水实验研究

铅锌矿在我国储存量大,电解法生产锌过程中可产生含Zn~(2+)、Pb~(2+)、Cd~(2+)、As5+和Cu~(2+)等重金属离子的漂洗废水。以硅藻土精土为基体,用碳酸钙作为改性剂制备改性硅藻土,对电解锌漂洗废水进行吸附实验研究。结果表明:在反应时间为150 min,碳酸钙改性硅藻土用量为3 g/L,pH为5.46,温度为25℃条件下,对废水进行吸附实验,吸附后废水中的Cu~(2+)和As5+离子浓度低于仪器检测线(0.01 mg/L和0.09 mg/L),Pb~(2+)浓度为0.16 mg/L,吸附后废水中Cu~(2+)、As5+和Pb~(2+)离子浓度均满足GB 25466—2010《铅锌工业污染物排放标准》的排放要求。同时,采用SEM、FTIR、XRD等对碳酸钙改性硅藻土进行表征,进一步探讨了碳酸钙改性硅藻土对重金属的吸附机理。     

温度对细菌碳酸酐酶催化碳酸钙沉积的影响

碳酸钙(CaCO3)沉积不仅在许多地质过程中起重要作用,而且在石刻文物和石质建筑物的修复以及环境治理等方面也有应用。CaCO3沉积过程在自然条件下极为缓慢,在CaCO3-H2O-CO2反应体系中CO2+H2OHCO3-+H+为限速步骤,可以利用生物催化剂来加速这一反应的进行。碳酸酐酶(Carbonic anhydrase,CA)是一种以锌为活性中心的金属酶,可以高效催化上述反应的进行,并在CaCO3沉积中具有显著促进作用。本文采用气体扩散体系,研究温度对典型细菌CA催化CaCO3沉积的速率及晶型晶貌的影响。结果表明,在实验温度(5～55℃)条件下,30℃时细菌CA催化沉积CaCO3的速率最快,而5℃时的沉积速率最慢,而且,温度会影响细菌CA催化形成的CaCO3晶体的大小和形貌。     

碳酸钙中的碳能被微藻利用吗

碳酸钙中的碳能否被微藻利用这一问题一直处于争论中。本文在开放与隔离空气CO2环境下用含有碳酸钙粉末和不同浓度乙酰唑胺的培养液培养衣藻和小球藻。通过双向同位素示踪技术,定量描述出不同条件下微藻对碳酸钙碳源的利用份额。在隔离空气CO2的环境下,微藻对碳酸钙碳源的利用份额明显大于开放环境下。在开放环境下,随着培养液中乙酰唑胺浓度增加,生物量减少,微藻对固有无机碳源的利用份额减少,对碳酸钙碳源的利用份额增加。在隔离空气CO2的环境下,随着培养液中乙酰唑胺浓度增加,微藻生物量增加,衣藻对固有无机碳源的利用份额增加,对碳酸钙碳源的利用份额减少,而小球藻反之。微藻主要是通过利用碳酸钙溶蚀的可溶性无机碳(DIC)这种间接方式来利用碳酸钙碳源。而外界大气CO2浓度和胞外碳酸酐酶是影响碳酸钙溶解的重要因素,因此其也明显的影响着微藻对碳酸钙碳源的利用。     

碳酸根对磷酸钙沉淀反应回收磷的影响简

以模拟的厌氧消化液为处理对象，通过小试实验，考察不同初始磷浓度C_P、Ca/P物质的量比、pH和温度下，碳酸根（CO₃^2-）对磷酸钙沉淀反应回收磷的影响；利用扫描电镜（SEM）、X射线衍射仪（XRD）和傅里叶变换红外光谱（FTIR）对沉淀产物进行表征。结果表明，高浓度的CO₃^2-对以磷酸钙沉淀反应去除和回收磷的效率影响较大；C_P相同时，CO₃^2-浓度（C_CO3^2-）越大，P的去除率越低，低C_P（20 mg/L）时尤为显著；当C_CO3^2-相同时，随着C_P的增大，反应速率加快，P的去除率逐渐升高，但升高幅度越来越小；增大Ca/P比和pH能提高P的去除率，降低CO₃^2-对磷酸钙沉淀反应的抑制作用，综合考虑实际效果，应选择Ca/P比为3.33，pH为9.0作为适宜的反应条件；升高温度对降低CO₃^2-对磷酸钙沉淀反应的抑制作用贡献不大。在C_P为60 mg/L，Ca/P比为1.67，pH为9.0，温度为20℃的条件下，当C _CO3^2-为0时，得到的沉淀产物主要为羟基磷灰石HAP；当C _CO3^2-为30 mmol/L时，得到的沉淀产物为磷酸钙和碳酸合磷灰石的混合物。     

Modeling the impacts of calcite precipitation on the epilimnion of an ultraoligotrophic, hard-water lake

A mass-balance model of calcite precipitation was developed to investigate the interactions of the varied processes governing the generation and fate of calcite in lakes. The model was used in conjunction with data to assess the evolution and impact of calcite precipitation for calcareous, ultraoligotrophic Torch Lake, Michigan (USA). This lake is an ideal setting for implementation of a baseline modeling study of calcite precipitation where the physical drivers could be evaluated without being dominated, as in many systems, by biological processes. The model provides a representation of calcite precipitation with particulate surface area changing over time, and demonstrates that it is possible for the change in water clarity to be explained by calcite precipitation employing standard optical models. Using the mass balance model to quantify the roles of the various chemical, biological and physical processes interacting in the lake's epilimnion, it was shown that the seasonal temperature rise and air-water CO₂ exchange drive calcite precipitation much more than primary production for this ultraoligotrophic system.     

Long-term depletion of calcium and other nutrients in eastern US forests

Both harvest removal and leaching losses can deplete nutrient capital in forests, but their combined long-term effects have not been assessed previously. We estimated changes in total soil and biomass N, Ca, K, Mg, and P over 120 years from published data for a spruce-fir site in Maine, two northern hardwood sites in New Hampshire, central hardwood sites in Connecticut and Tennessee, and a loblolly pine site in Tennessee. For N, atmospheric inputs counterbalance the outputs, and there is little long-term change on most sites. For K, Mg, and P, the total pool may decrease by 2%–10% in 120 years depending on site and harvest intensity. For Ca, net leaching loss is 4–16 kg/ha/yr in mature forests, and whole-tree harvest removes 200–1100 kg/ha. Such leaching loss and harvest removal could reduce total soil and biomass Ca by 20%–60% in only 120 years. We estimated unmeasured Ca inputs from rock breakdown, root-zone deepening, and dry deposition; these should not be expected to make up the Ca deficit. Acid precipitation may be the cause of current high leaching of Ca. Although Ca deficiency does not generally occur now in acid forest soils, it seems likely if anthropogenic leaching and intensive harvest removal continue.     

DRY STREAM REACHES IN CARBONATE TERRANES: SURFACE INDICATORS OF GROUND-WATER RESERVOIRS1

ABSTRACT: The method of identifying dry stream reaches in carbonate terrane as surface indicators of potential ground-water reservoirs offers a valuable exploration technique that is more rapid and less expensive than traditional exploration methods involving random test drilling. In areas where dry stream reaches occur, subsurface drainage successfully competes with surface drainage, and sheet-like dissolution openings have developed parallel to bedding creating the ground-water reservoir. The occurrence and hydraulic characteristics of such reservoirs are highly variable, as attested to by the wide range of well yields. Union Hollow in south-central Tennessee is the setting for a case study that illustrates the application of the dry stream reach technique. In this technique, dry stream reach identification is based on two types of readily acquired information: (1) remotely sensed black and white infrared aerial photography; and (2) surface reconnaissance of stream channel characteristics. Test drilling in Union Hollow subsequent to identification of the dry reach proved that a localized ground-water reservoir was present.