Thermal degradation of hexachlorobenzene in the presence of calcium oxide at 340–400 °C

Hexachlorobenzene (HCB) in the milligram range was co-heated with calcium oxide (CaO) powder in sealed glass ampoules at 340–400 °C. The heated samples were characterized and analyzed by Raman spectroscopy, elemental analysis, gas chromatography/mass spectrometry, ion chromatography, and thermal/optical carbon analysis. The degradation products of HCB were studied at different temperatures and heated times. The amorphous carbon was firstly quantitatively evaluated and was thought to be important fate of the C element of HCB. The yield of amorphous carbon in products increased with heating time, for samples treated for 8 h at 340, 380 °C and 400 °C, the value were 17.5%, 34.8% and 50.2%, respectively. After identification of the dechlorination products, the HCB degradation on CaO at 340–400 °C was supposed to through dechlorination/polymerization pathway, which is induced by electron transfer, generate chloride ions and form high-molecular weight intermediates with significant levels of both hydrogen and chlorine, and finally form amorphous carbon. Higher temperature was beneficial for the dechlorination/polymerization efficiency. The results are helpful for clarifying the reaction mechanism for thermal degradation of chlorinated aromatics in alkaline matrices.     

HT系列新型袋式除尘器在碳酸钙烘干机的应用

国内生产纳米级碳酸钙的企业大多选择三蒸往复式烘干机对一次脱水后的碳酸钙粉体进行脱水,烘干机排放的废气具有温度高、湿度大、气体含尘浓度高、粉尘粒径细微、易结晶等问题,为了能更好地处理废气中的粉尘,重点分析了碳酸钙生产企业纳米级烘干机排放气体的特性,结合旋风除尘器、静电除尘器、普通袋式除尘器在此行业中实际使用情况,进行分析和性能对比,重点说明HT系列新型袋式除尘器在碳酸钙行业的应用和特点.该类型除尘器既降低了设备投资成本,又实现了高效率回收、高标准排放.     

基于生物标志物法的珠江流域有机碳溯源及DIC施肥效应研究

内源有机碳由地表水体水生光合固定DIC产生,是岩石风化碳汇的重要组成部分。为准确区分河陆地流水体中的内源有机碳及计算其所占比例,本文选取珠江流域作为研究区,通过不同季节的野外采样调查,利用类脂生物标志物法,结合传统水化学特征,揭示河流中有机碳的来源差异;最终根据有机碳的时空分布规律与水-岩-土-气-生相互作用分析,明确流域岩性及气候变化对碳汇的影响。结果表明:(1)珠江流域水体中冬季和夏季内源有机碳占总有机碳比例的平均值分别为65%和54%,表明水生植物光合作用导致的初级生产力的重要性;(2)内源有机碳比例和水生藻类生物量与DIC浓度和呈现出显著的正相关关系,表明DIC对水生植物光合作用具有施肥效应;(3)雨季因降雨稀释DIC浓度和冲刷外源有机质,对水生植物的施肥效应减弱,生成的内源有机质减少,且携带的外源有机质增加,导致内源比例减少;(4)高悬浮质(TSS)可以遮挡水体表层太阳光,减弱水生光合作用强度,降低内源有机碳的形成;但在TSS浓度比较低的情况下,其对水生植物生长繁殖的影响则体现在为其提供空间和营养物,从而增加水生藻类生物量及内源有机碳比例。     

一种基于SDS溶液高效提取土壤残留Bt蛋白的方法

通过对SDS浓度、孵育温度和孵育时间3种提取条件的研究,建立了一种基于SDS溶液的提取土壤中残留Bt蛋白的方法(简称SDS法).在ρ(SDS)为2 g·L-1、孵育温度为50℃、孵育时间≥4 h条件下,采用SDS法可有效地从不同类型土壤样品中提取残留Bt蛋白,提取效果明显好于碳酸盐法、人造蠕虫肠道蛋白提取液法和PBST(phosphate buffer solution with Tween-20)法.     

化工厂场地酸化土壤工程化中和修复案例研究

对江苏某化工厂酸化地块进行了氧化钙中和修复工程研究。Ⅰ、Ⅱ、Ⅲ号地块剖面混合土样pH值分别为3.56、4.68和4.74,土壤修复目标定在pH值为6~8基本近中性。通过室内试验确定Ⅰ、Ⅱ、Ⅲ号地块土壤生石灰掺混比例为0.5%、0.3%和0.3%;现场中试后Ⅰ、Ⅱ、Ⅲ号地块石灰掺混比例调整为0.7%、0.35%和0.3%;中试结果用于场地机械搅拌工程修复,修复过程中定期随机采样对中和效果进行连续监测。监测结果基本达标后请第三方对修复效果进行评估,最后土壤回填压实。修复结果表明借助于科学的石灰添加量和工程机械混合措施,能快速有效地修复酸化地块土壤。     

Thermodynamics of NaHCO3 decomposition during Na2CO3-based CO2 capture

Amine-basedcarbon-capture technologies have been shown to be energetically expensive and to cause significant environmental and epidemiological impacts due to their volatility.Bicarbonate formation from carbon dioxide's reaction with water has been suggested as an effective alternative for capturing CO_2;however,the thermodynamics of this reaction are not well understood.This study experimentally determined the equilibrium constant of sodium bicarbonate(Na HCO_3)decomposition to sodium,water,and carbon dioxide;the study also compared the equilibrium constant to theoretical calculations.Using a combination of experimentation and thermodynamic relationships,the unitless equilibrium constants of the forward and reverse reactions were calculated accurately(error±9%and±4%,respectively).Equilibrium data were calculated using enthalpy and entropy values of each component of Na HCO_3decomposition at temperatures ranging from 25 to 155°C respectively.These results offer more data essential to optimizing Na HCO_3use in environmentally friendly nextgeneration CO_2-capture technologies.     

微生物诱导碳酸盐沉积介导的Cd2+固定

实验室条件下,研究了碳酸盐矿化菌施氏假单胞菌（Pseudomonas stutzeri）、枯草芽孢杆菌（Bacillus subtilis）和巴氏芽孢杆菌（Bacillus pasteurii）的生长对Cd²⁺的耐受性和固定效果,以及羟基磷灰石对3种菌固定Cd²⁺的影响,通过扫描电镜（SEM）、X射线能谱（EDS）、傅里叶红外光谱（FTIR）和X射线衍射（XRD）对碳酸盐矿化菌的诱导矿化产物进行了表征.结果表明,3种菌生长过程中B.pasteurii的脲酶活性最强,是P.stutzeri和B.subtilis脲酶活性的10倍左右,且P.stutzeri,B.subtilis,B.pasteurii产CO₃^2-的最高浓度分别为588.19,661.72,1735.18mg/L,培养体系中pH值均呈现升高的趋势,最高pH值分别为8.23,9.06,9.52;Cd²⁺浓度在0~10mg/L范围内对P.stutzeri的生长影响较小,而当Cd²⁺浓度高于1mg/L时则会抑制B.subtilis和B.pasteurii的生长.初始Cd²⁺浓度为0.5mg/L时,培养120h,P.stutzeri,B.subtilis和B.pasteurii对Cd²⁺的固定去除率分别为96.37%,99.40%,97.57%;加入羟基磷灰石能够提高碳酸盐矿化菌对Cd²⁺的去除率.SEM和EDS结果显示,P.stutzeri和B.subtilis诱导形成的矿化产物多聚集在菌体周围或附着在菌体表面,呈球状或网状结构,表面疏松多孔,B.pasteurii的矿化产物附着在菌体表面,结构致密,呈不规则的球状;FTIR分析表明矿化产物中存在CO₃^2-,结合XRD结果,证实3种菌诱导沉淀矿化产物主要是CaCO₃,而Cd²⁺与Ca²⁺会以同晶置换的方式形成CdCO₃晶体,B.pasteurii在诱导矿化的过程中可将Cd²⁺以Ca_0.67Cd_0.33CO₃共沉淀的方式固定.     

Chemical Tracking and Marine Environmental Impact of Ocean Disposal of Calcium Carbonate Residue in the North Yellow Sea

The objective of this study is to determine the sedimentation rate and dispersion area of calcium carbonate residue dumped at sea and the impact to marine environment of dumping by a laboratory simulation experiment; chemical tracking in the field with the help of acoustic and optical tracking; and a comparative study of baseline conditions and marine environmental impact after dumping. Turbidity, pH and phosphate are selected as the chemical tracers to be monitored.

Results show that in the dumping area of 15 square miles with water depth of 50 m, if 217 t calcium carbonate residue is dumped (spot dumping) in the presence of a pycnocline with a current velocity of 60 cm/s (close to the maximum) the maximum dispersion distance of the calcium carbonate residue plume front is less than 2100 m; the dispersion area is less than 0.56 km²; and the maximum dispersion time is about 60 min when the turbidity and pH in the whole dispersion area return to background level. Therefore, the ocean disposal of calcium carbonate residue is feasible.     

以膨润土为载体的碳酸盐吸收剂对二氧化碳的吸收

采用膨润土为载体,KHCO3为前驱物通过喷雾-干燥法制成固体碳酸钾吸收剂,制成的固体吸收剂粒径大小为0.5—2.0 mm,密度为1.73 g.mL-1.通过K2CO3负载量、吸收温度、吸收时间、床层纵横比等因素考察固体吸收剂对CO2气体的吸收效率及循环反应特性.分析碳酸钾吸收剂对CO2的吸收机理,并与以碳酸氢钠为前驱物制备的吸收剂进行对比,比较两种吸收剂对CO2吸收效果的差异性.通过XRD测试吸收剂吸收反应前后组成的变化,BET多点法测试吸收剂比表面积,扫描电镜观察吸收剂表面形态特征.结果表明,碳酸钾吸收剂和碳酸钠吸收剂对CO2气体均具有较高的吸收量,相比而言碳酸钾吸收剂的碳酸化反应速率较快,而且经过多次循环反应后吸收效果未发生衰减,在60℃—80℃范围内,碳酸钾吸收剂对CO2的吸收能力最佳.     

石漠化地区豆科植物根瘤菌降解碳酸钙、镁能力研究

微生物对岩溶地区岩石风化、成土具有明显的促进作用,为了筛选出能够促进碳酸盐岩风化、加快成土速率的优势根瘤菌菌株,将其与豆科植物建立共生体系,进行石漠化地区修复与治理,实验以分离自云南石漠化地区的9株豆科植物根瘤菌为研究对象,将9株根瘤菌接种于加有难溶性碳酸钙或碳酸镁的液体培养液中,28.5℃、160 r·min-1摇床培养15 d,于0、1、3、6、10、15 d取样2 mL,每个样3个平行;将样品加入到10 mL体积比5∶1的硝酸高氯酸消化液中浸泡过夜,放在电热板上缓慢加热至溶液澄清透明,分别用含La3＋2%的盐酸溶液定容至10 mL,空白用同样方法处理;最后采用原子火焰吸收方法测定样品中Ca2＋和Mg2＋含量,筛选出对碳酸盐岩主要成分碳酸钙和碳酸镁具有强降解作用的根瘤菌菌株。结果表明：热带根瘤菌Rhizobium tropici （SWFU09）和根瘤菌Rhizobium sp.（SWFU02）对碳酸钙降解作用最强;对碳酸镁降解作用最好的菌株为根瘤菌Rhizobiumsp.（SWFU03）、热带根瘤菌Rhizobium tropici（SWFU05）和慢生根瘤菌Bradyrhizobium sp.（SWFU01）。溶液pH值对碳酸镁降解作用具重要的影响,对碳酸钙降解作用影响不大,说明根瘤菌代谢产生的酸性物质（有机酸、氨基酸）对碳酸钙和碳酸镁降解作用有一定影响,但不是唯一影响因素;也可能是微生物代谢产生的有机配体（基）吸附碳酸钙和碳酸镁表面,与水体中的成分形成复合物,改变溶解的平衡,置换出Ca2＋和Mg2＋。