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141.
为考察土壤锰氧化物的还原溶解行为,本文选取常见的根系分泌的8种有机酸(抗坏血酸、香草酸、柠檬酸、草酸、酒石酸、水杨酸、半胱氨酸和邻苯二甲酸)和1种酚类化合物(邻苯二酚),人工合成的Mn O2和5种富含氧化锰的土壤(广东徐闻的砖红壤、海南澄迈的砖红壤、云南昆明的砖红壤、浙江嵊县的红壤和江苏南京的黄棕壤),研究了有机化合物对氧化锰的还原溶解作用.结果表明,较低p H和较高温度有利于有机化合物对Mn O2的还原溶解.在p H 4.5—5.5和温度5—45℃范围内,不同有机化合物还原溶解Mn O2能力的大小顺序为:邻苯二酚半胱氨酸抗坏血酸香草酸柠檬酸草酸≈酒石酸水杨酸≈邻苯二甲酸.邻苯二酚、半胱氨酸和抗坏血酸对土壤中氧化锰也有较强的还原溶解能力.当5种土壤比较时,徐闻砖红壤中还原溶解出的锰量最高,其次为昆明砖红壤,嵊县红壤中还原溶解出的锰量最小.当有还原性有机化合物存在时徐闻砖红壤、昆明砖红壤和澄迈砖红壤中的氧化锰容易发生还原溶解反应,增加土壤中可溶态和交换态Mn2+的含量,并可能对植物产生锰毒害. 相似文献
142.
In order to search the degradability of kraft lignin, the potential bacterial strains Bacillus subtilis (GU193980) and Klebsiella pneumoniae (GU193981) were isolated, screened and applied in axenic and co-culture conditions. Results revealed that mixed culture showed better decolorization efficiency (80%) and reduction of pollution parameters (COD 73% and BOD 62%) than axenic culture. This indicated syntrophic growth of these two bacteria rather than any antagonistic effect. The HPLC analysis of degraded samples of kraft lignin has shown the reduction in peak area compared to control, suggesting that decrease in color intensity might be largely attributed to the degradation of lignin by isolated bacteria. Further, the GC–MS analysis showed that most of the compounds detected in control were diminished after bacterial treatment. Further, the seed germination test using Phaseolus aureus has supported the detoxification of bacterial decolorized kraft lignin for environmental safety. All these observations have revealed that the developed bacterial co-culture was capable for the effective degradation and decolorization of lignin containing rayon grade pulp mill wastewater for environmental safety. 相似文献
143.
144.
145.
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。 相似文献
146.
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。 相似文献
147.
Pseudomonas sp. QJX-1的锰氧化特性研究 总被引:2,自引:2,他引:0
从锰矿土壤样品中分离、纯化出1株高效锰氧化细菌(QJX-1),经16S rDNA序列鉴定为Pseudomonas sp.QJX-1.研究表明,Pseudomonas sp.QJX-1含有锰氧化的必需成分多铜氧化酶基因CumA,当初始Mn2+为5.05 mg·L-1,菌密度D600为0.020时,该菌可在48 h内将Mn2+转化,且转化率高达99.4%.在寡营养条件下该菌锰氧化速率较富营养条件下有显著提高;添加石英砂滤料促使生物膜的快速形成,进而促进Mn2+的生物转化.根据研究结果推测地下水处理过程中生物锰氧化速率较快. 相似文献
148.
利用从土壤铁锰结核中分离筛选得到的1株锰氧化细菌(芽孢杆菌,Bacillus sp.)GY16合成生物氧化锰,与化学合成的水钠锰矿进行比较,研究了不同氧化锰对As的氧化吸附特征.结果表明,生物氧化锰和化学氧化锰对As(Ⅲ)均有强烈的氧化作用,化学氧化锰对As(Ⅲ)的氧化速率要高于生物氧化锰,而单位物质的量的生物氧化锰对As(Ⅲ)的氧化量可达化学氧化锰的5倍,并且对As(Ⅴ)有非常明显的吸附作用,而化学氧化锰对As(Ⅴ)的吸附量则非常少.此外,随着生物氧化锰与As(Ⅲ)/As(Ⅴ)反应的进行,生物氧化锰对As(Ⅲ)/As(Ⅴ)的氧化吸附速率均逐渐降低.随着pH的增加,生物氧化锰对As(Ⅲ)的氧化量及As(Ⅴ)的吸附量均呈现出明显的下降趋势,但是化学氧化锰对As(Ⅴ)的吸附量却有微弱的增加.研究结果可为生物氧化锰应用于环境修复提供可靠的技术支撑. 相似文献
149.
An investigation of cellular distribution of manganese in hyperaccumlator plant Phytolacca acinosa Roxb. using SRXRF analysis 总被引:1,自引:0,他引:1
XU Xiang-hu SHI Ji-yan CHEN Ying-xu XUE Sheng-guo WU Bei HUANG Yu-ying 《环境科学学报(英文版)》2006,18(4):746-751
Phytolacca acinosa Roxb. (P acinosa) is a recently discovered manganese hyperaccumulator plant from southern China. It is a good candidate for phytoremediation of manganese(Mn) polluted soil for its high biomass and fast growth. Knowledge of the tissue localization and identification of heavy metals can provide essential information on metal toxicity and bioaccumulation mechanisms. Synchrotron radiation X-ray fluorescence spectroscopy (SRXRF) microprobe was used in this study to investigate the cellular distributions of Mn and other elements in root, stem, leaf, petiole and midrib of P. acinosa. The highest Mn content was found in the vascular tissues of root, stem, petiole and midrib. Cortex in root played a key role in Mn absorption and Mn was limited in the vascular bundle during the process of transportation in stem. Moreover, Mn content in leaf epidermis was higher than that in mesophyll, which suggested that the sequestration of Mn in leaf epidermis might be one of the detoxification mechanisms of P. acinosa. The significance of other elemental (such as P, S, K, Ca, Fe, Zn and Cu) distribution patterns and the correlation with Mn were also discussed. 相似文献
150.
Biogeochemical reductive dechlorination (BiRD) is a newly recognized method for the remediation or natural attenuation of chlorinated solvents. Chlorinated solvents are rapidly treated by abiotic reaction with reduced mineral iron sulfides. Iron sulfides are formed by naturally occurring sulfate-reducing bacteria when sufficient SO(4)(2-) and organic carbon are present or supplied to sediments containing mineral iron. An example of site characterization focusing on BiRD is presented focusing on mineral phases. Methods demonstrated here may be employed at other sites to evaluate naturally occurring BiRD or to evaluate an engineered BiRD remediation. A field investigation was performed at a TCE contaminated site at Altus AFB with naturally high concentrations of SO(4)(2-) and Fe(III) minerals and where an accidental fuel spill provided organic carbon. In the area of this fuel spill significant mineral iron sulfides were found, sulfate was almost completely removed, and TCE was absent. Only small amounts of daughter products were found, further indicating that the BiRD pathway was operative. Mass balance data indicates all of the remaining TCE (182 kg) could be treated by the remaining FeS (66.5 kg) in the upper aquifer; however, the FeS was not co-located with TCE to enable complete reaction. Laboratory microcosm tests with FeS amended and FeS-rich sediment from Altus AFB also suggest that BiRD is capable of destroying TCE. The results suggest that an engineered BiRD treatment is possible for this site. 相似文献