基于能值分析的煤炭矿区复合生态系统评价

煤炭矿区复合生态系统评价是对其进行有效管理及调控的手段之一。研究了煤炭矿区复合生态系统内涵,剖析了煤炭矿区复合生态系统的典型特征,论述了运用能值分析方法评价复合生态系统的特殊性;进而,构建了煤炭矿区复合生态系统及其子系统的能值评价指标。选择山东省龙口矿区北皂煤矿为研究对象,进行了实证研究。应用实际数据,测算了2006—2012年复合生态系统及子系统各个能值评价指标。研究结果表明,能值理论与能值分析是评价煤炭矿区复合生态系统的有效方法,各项指标变化反映了复合生态系统的演进趋势;不可再生煤炭资源的过度消耗、可再资源利用率低是这一系统的典型特征;能值评价指标的测算结果表征环境子系统负荷较小。研究结果可为实施有效的煤炭矿区复合生态系统管理提供智力支持和决策参考依据。     

东部草原露天矿区粘土改良模拟研究

以我国东部草原露天矿区粘土为研究对象,采用盆栽试验方法,以粘土与表土和沙土混合物为培养基质,三叶草(Trifolium repens Linn)为供试植物,研究不同比例下三叶草生物量、养分吸收量、土壤理化和生物学性状的差异,为寻找最佳配比提供依据。结果表明:不同混合比例显著影响三叶草生物量,粘土+表土(1∶1、1∶2和1∶3)生物量最高(26.5—40.0 g/盆),平均为31.2 g/盆,粘土+沙土(1∶1、1∶2和1∶3)次之(14.9—20.3 g/盆),平均为18.9 g/盆,粘土、沙土和表土平均分别是9.0、5.4 g/盆和41.7 g/盆,同样地,粘土+表土混合基质上三叶草氮吸收量平均为1071 mg/盆,分别是粘土+沙土、粘土和沙土氮吸收量660、321 mg/盆和190 mg/盆的1.62、3.34倍和5.64倍,磷和钾吸收量具有相似变化规律,这与三叶草根直径、根长、根表面积和根尖数有显著关联性;粘土和表土与粘土和沙土混合基质的容重和最大持水量分别显著下降7.4%—21.5%和24.5%—71.8%,饱和入渗率、孔隙度和标准化平均重量直径分别显著增加26.9%—96.3%、45%—218%和34%—72%;全氮、有机质、速效磷、速效钾、饱和电导率显著增加23.0%—88.3%、25.1%—146%、44.0%—91.5%、70.3%—114.8%和3.5%—59.3%;磷酸酶、脲酶、蔗糖酶、硝酸还原酶和固氮酶活性显著提高45.5%—105%、65.2%—172.3%、160%—252%、53.4%—62.7%和197%—374%;真菌、细菌和放线菌数量增幅为119%—142%、93.5%—107%和83%—147%。相关性分析表明,生物量与土壤理化性状、酶活性和微生物数量呈显著或极显著正相关,表现为粘土+表土=表土粘土+沙土粘土沙土。因此,表土或沙土均能改良粘土性状,其中粘土和表土1∶2配比效果最优。     

Nutrient limitation of algal periphyton in streams along an acid mine drainage gradient

Metal oxyhydroxide precipitates that form from acid mine drainage (AMD) may indirectly limit periphyton by sorbing nutrients, particularly P. We examined effects of nutrient addition on periphytic algal biomass (chl a), community structure, and carbon and nitrogen content along an AMD gradient. Nutrient diffusing substrata with treatments of +P, +NP and control were placed at seven stream sites. Conductivity and SO₄ concentration ranged over an order of magnitude among sites and were used to define the AMD gradient, as they best indicate mine discharge sources of metals that create oxyhydroxide precipitates. Aqueous total phosphorous (TP) ranged from 2 to 23 μg · L^?1 and significantly decreased with increasing SO₄. Mean chl a concentrations at sites ranged from 0.2 to 8.1 μg · cm^?2. Across all sites, algal biomass was significantly higher on +NP than control treatments (Co), and significantly increased with +NP. The degree of nutrient limitation was determined by the increase in chl a concentration on +NP relative to Co (response ratio), which ranged from 0.6 to 9.7. Response to nutrient addition significantly declined with increasing aqueous TP, and significantly increased with increasing SO₄. Thus, nutrient limitation of algal biomass increased with AMD impact, indicating metal oxyhydroxides associated with AMD likely decreased P availability. Algal species composition was significantly affected by site but not nutrient treatment. Percent carbon content of periphyton on the Co significantly increased with AMD impact and corresponded to an increase in the relative abundance of Chlorophytes. Changes in periphyton biomass and cellular nutrient content associated with nutrient limitation in AMD streams may affect higher trophic levels.     

基于水足迹理论的煤制油产业布局评价

煤制油是我国应对石油危机的重要途径之一,但其高耗水的特点使其备受争议。利用水足迹理论对全国五大煤炭基地2015年规划的煤制油产业进行了蓝水足迹和灰水足迹的测算,分析了煤制油产业对这些区域水资源的耗用情况及冲击程度。结果显示,神东、晋东和新疆伊犁3个基地的煤制油产业蓝水足迹超过了1亿t、灰水足迹超过了3亿t,其中神东地区作为最大的煤制油产地两项数值分别达到1.9亿t和4.1亿t与当地水资源总量对比,宁东地区煤制油耗水冲击最大,占当地水资源总量的28.2%;新疆伊犁地区比例最小,为0.36%。通过对这5个煤炭基地以区域为尺度的水足迹结构分析和评价比较,得出了两种煤制油工艺的水资源消耗差异,并且为煤制油产业在五大基地的合理布局给出了依据,与此同时为接下来煤制油产业的技术革新和流程优化也提出了相应的建议。     

不同风化程度钾长石表面矿物分解细菌的筛选及遗传多样性

【目的】不同风化程度钾长石表面矿物分解细菌生物多样性研究将有助于了解矿物生物风化、生物成矿和土壤形成的演化规律和机理。【方法】采用纯培养法自南平钾矿区高、中、低风化度钾长石以及矿区土壤样品中分离矿物分解细菌,通过摇瓶释硅实验比较不同菌株分解矿物能力,采用16SrDNA限制性酶切多态性分析(Amplified rDNA Restriction Analysis,ARDRA)研究了供试菌株的遗传多样性。【结果】分离筛选到35株生长良好的矿物分解细菌,与对照相比,接菌处理发酵液中有效硅增加了101～206%;所有供试菌株可分为11个OTU,分别属于5个门,6个科,7个属。多数菌株(74%)属于γ-变形杆菌纲(γ-Proteobacteria)。泛菌属(Pantoea),沙雷氏菌属(Serratia),假单胞菌属(Pseudomonas)为优势种群。【结论】南平钾矿区矿物分解细菌具有丰富的微生物种群多样性,且γ-变形杆菌纲(γ-Proteobacteria)细菌在钾长石风化过程中可能起了重要的作用。     

A Novel Community of Acidophiles in an Acid Mine Drainage Sediment

A sediment sample (pH 2.5) was collected at an acid mine drainage site in Anhui, China. The present acidophilic microbial community in the sediment was studied with a 16S rRNA gene clone library. Small-subunit rRNA genes were PCR amplified, cloned and screened by amplified rDNA restriction analysis (ARDRA). Subsequently, 10 different clones were identified and they were affiliated with Acidobacteria, β/γ-Proteobacteria, δ-Proteobacteria, Nitrospira, Candidate division TM7, and Low G + C Gram-positives. Phylogenetic analysis of 16S rRNA gene sequences revealed a diversity of acidophiles in the sediment that were mostly novel. Unexpectedly, 16S rRNA gene sequences affiliated with δ-Proteobacteria were found to constitute more than 60% of clone library. To our knowledge, this is the first occasion that bacteria of δ-Proteobacteria have been found dominant in the acidic habitat. Anaerobic sulfate- or metal reduction is the predominant physiological trait of bacteria of this subdivision. The high sulfate, ferric iron and the presence of bioavailable carbon in the anaerobic microenvironment may result in the dominance of bacteria of δ-Proteobacteria.     

In-Situ Remediation of Lead–Zinc Polymetallic Mine Contaminated Soils by MnFe2O4 Microparticles

In-situ remediation is a practical approach to remediate soils contaminated with heavy metals. The MnFe₂O₄ microparticles (MM) were prepared for the in-situ remediation of contaminated soils from a lead–zinc polymetallic mine in Inner Mongolia province, China. The effects of MM dosage, pH on remediation efficiency, were determined with static vibration leaching experiment, and the release risk of heavy metals of treated soil was studied by column leaching experiment. The results showed that the leached Cu, Pb, Zn, and As concentration decreased drastically with increasing MM dosage, when the dosage was lower than 10 g/kg. Moreover, the decrease of pH caused increase of leached concentration of Cu, Pb, Zn, but slight decrease of leached As concentration. For the amended soil, concentrations of leached heavy metals were lower than Grade III limit of Chinese Environmental Quality Standards for Ground and Surface water (GB3838-2002) under simulated acid rain leaching condition. In comparison with non-amended soils, the total amount of Cu, Pb, Zn, and As release from amended soils was reduced by 93.6%, 69.2%, 57.0%, and 99.7%, respectively. The MM is a kind of promising amendment for heavy metals contaminated soil.     

Fe- and S-Metabolizing Microbial Communities Dominate an AMD-Contaminated River Ecosystem and Play Important Roles in Fe and S Cycling

Indigenous Fe- and S-metabolizing bacteria play important roles both in the formation and the natural attenuation of acid mine drainage (AMD). Due to its low pH and Fe-S-rich waters, a river located in the Dabaoshan Mine area provides an ideal opportunity to study indigenous Fe- and S-metabolizing microbial communities and their roles in biogeochemical Fe and S cycling. In this work, water and sediment samples were collected from the river for physicochemical, mineralogical, and microbiological analyses. Illumina MiSeq sequencing indicated higher species richness in the sediment than in the water. Sequencing also found that Fe- and S-metabolizing bacteria were the dominant microorganisms in the heavily and moderately contaminated areas. Fe- and S-metabolizing bacteria found in the water were aerobes or facultative anaerobes, including Acidithiobacillus, Acidiphilium, Thiomonas, Gallionella, and Leptospirillum. Fe- and S-metabolizing bacteria found in the sediment belong to microaerobes, facultative anaerobes, or obligatory anaerobes, including Acidithiobacillus, Sulfobacillus, Thiomonas, Gallionella, Geobacter, Geothrix, and Clostridium. Among the dominant genera in the sediment, Geobacter and Geothrix were rarely detected in AMD-contaminated natural environments. Canonical correspondence analysis indicated that pH, S, and Fe concentration gradients were the most important factors in structuring the river microbial community. Moreover, a scheme explaining the biogeochemical Fe and S cycling is advanced in light of the Fe and S species distribution and the identified Fe- and S-metabolizing bacteria.     

Effect of Organic Residues and Liming Materials on Metal Extraction from a Mining-Contaminated Soil

Incubation tests were used to assess the effectiveness of three different organic residues and three different liming materials, alone or in combination, in the remediation of a mine contaminated soil. The organic residues tested were sewage sludge from a municipal wastewater treatment plant (SS), compost from the organic fraction of unsorted municipal solid waste (MSWC), and garden waste compost (GWC), applied at 100 and 200 Mg ha^{? 1}. The liming materials tested were agriculture limestone (6.4 Mg ha^{? 1}), calcium oxide (3.7 Mg ha^{? 1}), and sugar beet sludge (12.2 Mg ha^{? 1}) from the sugar manufacturing process. The soil and mixtures of soil and amendments were adjusted to 70% of the maximum water holding capacity and incubated for 28 days in a controlled-temperature room at 20°C ± 1°C. At the end of the incubation, samples were analyzed for pH, electrical conductivity, organic matter content, CaCl₂-extractable, and' NH4Ac/HAc+ EDTA–extractable metal fractions (Cu, Zn, and Pb). Correlations among the variables and/or similarities among the treatments were identified by principal component analysis and hierarchical cluster analysis. The amendments tested decreased the CaCl₂-extractable Cu and Zn fractions, considered as mobile metal fractions, to below analytical detectable limits, providing organic matter to the soil with levels between 1% and 2% at the end of the experiment, significantly different relatively to the original soil. pH and electrical conductivity reached high values when using 200 Mg ha^{? 1} SS or 200 Mg ha^{? 1} MSWC, with any of the liming materials tested, making these application rates excessive for this particular situation. Furthermore, the treatments using MSWC increased the NH4Ac/HAc+ EDTA–extractable Cu, Pb, and Zn fractions, considered as mobilizable metal fractions, as did the 200 Mg ha^{? 1} SS for Pb and Zn. Considering the overall results, the compost made from garden waste decreased metal solubility in the soil and increased soil pH and organic matter content, without the addition of large amounts of soluble salts, and without increasing the mobilizable metal content. Of the organic materials tested, this was the only one that can be considered adequate for remediation of the contaminated soil under study, at the application rates tested.