草酸盐介导下含As(V)黄钾铁矾的相转化过程与As(V)的再分配行为

黄钾铁矾能够通过吸附和共沉淀作用固定酸性矿山废水（AMD）中的重（类）金属（如砷）,降低其迁移性和生物可利用性.草酸盐广泛存在于天然水环境中,其具有的羧酸官能团能改变铁矿物的稳定性,进而影响吸持的重（类）金属的再分配行为.利用水热法合成含As（V）黄钾铁矾,探究其在不同草酸盐浓度与pH条件下的溶解、重结晶和共沉淀As（V）的行为.研究结果表明,草酸盐与含As（V）黄钾铁矾表面Fe（III）活性位点配位形成的可溶性强络合物是促进矿物溶解的第一步和关键;在pH 2.5时,含As（V）黄钾铁矾的溶解速率随草酸盐浓度增加而增加,伴随大量As（V）释放到溶液,反应过程中只有少量As（V）重新吸附到固相上,这是由于草酸盐与As（V）竞争矿物表面的同一活性位点;在pH 6.5条件下,草酸盐促进含As（V）黄钾铁矾的重结晶,经X射线衍射分析表明针铁矿和纤铁矿为主要产物,能有效地吸附释放的As（V）.研究结果有助于揭示在AMD环境下黄钾铁矾沉积物与含羧酸官能团有机酸共存时对As（V）的释放和固定机理,对AMD环境中As（V）污染控制有重要意义.     

生活垃圾焚烧飞灰矿物学特性及重金属分布

生活垃圾焚烧飞灰的矿物学特性是飞灰中重金属赋存环境的直观反映,与重金属在处置环境中的释放和迁移行为密切相关.为掌握重金属在生活垃圾焚烧飞灰中的分布规律,结合X射线衍射、扫描电镜等常规矿物学研究工具及矿物解离分析系统对飞灰的矿物学宏观属性和微观属性进行全面测试.结果表明,飞灰是由矿物相和非矿物相组成,两者之间紧密连生,主要矿物相包括氯盐和方解石、氢氧钙石等多种含钙矿物.重金属元素在飞灰中主要以3种形式存在:均匀分布在无定形的非矿物组分中,以同晶置换赋存在方解石等矿物中以及吸附在特殊矿物如石英、赤铁矿等表面.难挥发性重金属Cu和Cr绝大部分分布在非矿物相中;半挥发性重金属Zn和Cd各有43.92%和60.61%的含量分布在矿物相中,其中,方解石对Cd、赤铁矿对Cr及硅酸盐对Zn存在较强的富集作用.     

Influence of Suspended Clay Minerals and Humic Matter on the Solid Phase Extraction Efficiency of Selected Pesticides from Water

The purpose of this investigation was to determine the influence of humic acids (HA) and Ca-montmorillonite (CaM) on the solid-phase extraction (SPE) efficiency of atrazine, alachlor and α-cypermethrin from water samples at various pH-values. The nature and intensity of binding of the studied pesticides to CaM were determined by X-ray diffraction analysis and termogravimetric analysis (TGA) test. The studied pesticides eluted from discs were analysed by thin-layer chromatography (TLC). The effects of CaM and humic acid were generally pH-dependent and acted independently in extraction efficiency influence. Lower recovery of pesticides was observed at higher pH values when CaM was ≥0.1 g and was attributed to greater dispersion of clay, increased surface area and subsequent adsorption. Concentrations of dissolved organic carbon (DOC) in humic acid had less effect on the extraction efficiency when water was at pH 8 compared to water at pH 2, which was probably due to greater nonpolar interactions of the pesticides to the charge-neutralized humic acid molecule.     

封存过程中CO2流体与煤中矿物作用关系研究进展

利用深部煤层封存二氧化碳(CO2),既能减排主要人为温室气体CO2,又能同步开采煤层气(主要成分为甲烷,即CH4)。在适宜CO2封存的含煤储层条件下,CO2属于超临界流体,其易与煤中部分无机矿物发生作用,进而改变煤的理化性质,最终影响煤层的CO2封存效果。为此,归纳了煤中易与CO2发生作用的矿物分布特征,分析了CO2与矿物间的作用规律及其对煤理化性质的影响,并指出了后续研究方向。结果表明,煤中易与CO2流体发生作用的无机矿物主要包括碳酸盐矿物和黏土矿物。上述矿物的分布与煤变质程度和沉积环境有关。在封存过程中,超临界CO2流体与煤中矿物间的作用会改变煤体孔隙结构、煤的CO2吸附能力和含煤储层渗透率。针对CO2与煤中矿物的作用关系,后续需开展以下研究:CO2流体与煤中矿物之间的微观作用机理;CO2流体与煤层顶底板中主要无机矿物的作用规律;实际储层条件(温度、压力和地应力等)对CO2与矿物之间作用关系的影响;CO2与矿物之间的相互作用对同步采收CH4的影响。     

Variation of crack intensity factor in three compacted clay liners exposed to annual cycle of atmospheric conditions with and without geotextile cover

Performance of compacted clay liners commonly used as landfill barrier systems can be subject to decline in terms of hydraulic conductivity if left exposed to atmospheric conditions for an extended period of time prior to placement of overlaying layers. The resulting desiccation cracking can lead to increased hydraulic conductivity. Desiccation crack intensity was studied for three clayey soils commonly used for construction of landfill barrier system in a relatively large scale test setup exposed to real time atmospheric conditions over a complete annual cycle. A white separator geotextile cover was presumed to be capable of reducing the intensity of desiccation cracking through absorbing and maintaining higher amounts of moisture and reducing the temperature of the soil surface in comparison to a directly exposed soil surface. Desiccation cracking was monitored using a digital imaging technique for three compacted clay liners in two sets, one open to air and the second covered with the white geotextile. Crack intensity factor approached a relatively stable phase after certain cycles corresponding to atmospheric dry wet cycles. The results indicated that the white separator geotextile was capable of reducing the crack intensity factor by 37.4–45.9% throughout the experiment including the cyclic phase of desiccation cracking. During the stable phase, the maximum reduction in crack intensity factor of 90.4% as a result of applying geotextile cover was observed for the soil with the lowest plastic index and clay content and therefore the lowest magnitude of crack intensity factor. The other two soils with similar clay content but different plastic index showed 23.6% and 52.2% reductions in crack intensity factor after cyclic phase when covered with geotextile.     

碳酸盐-硫酸盐矿物强化垃圾渗滤液厌氧处理研究

厌氧消化通常是垃圾渗滤液生物处理的首要环节,但处理效率不高.本研究尝试通过添加碳酸盐、硫酸盐等矿物来提高垃圾渗滤液的厌氧转化效率.研究共设置5组厌氧生物反应器,包括投加硬石膏、方解石、石膏、白云石的反应器及空白对照,考察添加矿物对垃圾渗滤液厌氧消化的影响.从实验结果可以看出,添加矿物的反应器中COD的去除率可以达到75%左右,而空白对照组去除率尚不足60%,添加矿物反应器甲烷产量显著高于对照.从反应器中的p H变化可以看出,矿物的添加可以提高溶液中的p H.研究结果表明,添加碳酸盐/硫酸盐矿物对垃圾渗滤液中的有机物厌氧消化过程具有重要的促进作用.     

垃圾填埋场甲烷厌氧氧化作用研究进展

垃圾填埋场是温室气体甲烷的重要人为排放源之一,垃圾分解产生的甲烷会发生垂向和侧向迁移,并被氧化固定在垃圾填埋场中。研究显示与硫酸盐还原作用耦合的甲烷厌氧氧化(AOM)作用在垃圾填埋场内及其渗滤液羽状体中均可发生,形成自生碳酸盐和硫化物等沉积。因此,AOM作用是垃圾填埋场甲烷减排的重要途径之一。然而只运用气体地球化学方法与技术难以确定填埋场AOM作用的特征,而填埋场内自生碳酸盐可能保存了AOM作用的信息,但其矿物学、地球化学等特征很少有报导,还有待进一步研究确定。     

天山北麓宁家河阶地上的黄土堆积及其磁学特征

本文报道了新疆地区天山北麓宁家河阶地上的黄土堆积。研究剖面的两层黄土为河流 砾石层所隔开,这在新疆地区较为少见。通过系统的岩石磁学和粒度测量,分析了该剖面两层 黄土的磁学特征,并初步探讨磁化率变化机制。结果表明：黄土中的主要磁性矿物为磁铁矿和 磁赤铁矿,并含有少量赤铁矿和针铁矿。亚铁磁性矿物主要以多畴（MD）、假单畴（PSD）颗 粒为主,反映了这一地区极弱的成土作用。砾石层上下两层黄土磁学性质存在着差异,表现为 上层黄土具有较高的磁性矿物含量、较粗的磁颗粒和相对含量较高的软磁性矿物。下层黄土受 到后期河水的改造可能是导致这些差异的原因。磁化率与粒度呈现较好的正相关关系,与黄土 高原的情况相反,说明干旱地区的黄土磁学性质主要受原生磁性矿物控制。搬运风力和源区变 化是磁化率变化的主导因素。     

铈插层黏土负载铁催化剂在H2S选择性催化氧化过程中催化性能的研究

合成了铈插层的Laponite黏土材料(Ce-Lap),并以此材料为载体,分别负载质量分数为3%、5%、8%、10%的Fe制备Fe/Ce-Lap催化剂,通过XRD、氮气吸脱附曲线、XRF、TG、FT-IR、O2-TPD、H2-TPR、XPS等手段,对催化剂的物理化学性质进行了表征测试,并考察了催化剂在H2S选择性催化氧化反应过程中的活性.结果表明,5%的Fe/Ce-Lap在180℃时表现出最好的催化活性,能达到96%的硫产率,这归因于Fe与Ce之间的相互作用,改善了Fe3+的氧化还原能力.此外,较高的氧吸附能力及铁物种的高分散度促进了氧化反应的进行.