安太堡露天矿南排土场滑体植被治理技术

论述了安太堡矿南排土场滑体整治模式,通过植被减少滑体侵蚀及水土流失,改善了滑体的生态景观,对滑体安全起到了良好作用。     

粉煤灰对矿井水中重金属离子的吸附研究

本文通过静态热力学实验的方法，研究了粉煤灰对矿井水中Ｐｂ＾２＋，Ｚｎ＾２＋，Ｃｕ６２＋等重金属离子的吸附性能。着重分析了ＰＨ值，吸附时间，粉煤灰活化程度等因素对其吸附能力的影响。     

Preconcentration and determination of trace copper(II) in natural water using silica gel modified with 1-(2-pyridylazo)-2-naphthol

Trace copper (II) in water can be preconcentrated using silica gel modified with 1-(2-pyridylazo)-2-naphthol (PAN) and be determined spectrophotometri-cally. The conditions for the preconcentration were studied. The method was applied to both artificial and natural water samples and the results suggest that copper (II) of ppb level in water can be measured accurately after the preconcentration.     

萝北县矿山企业的环境问题与整治对策

萝北县矿产资源丰富,矿山开采遍布北部山区,对环境造成一定的破坏.本文分析了环境破坏的原因,提出了整治对策.     

大庆红岗生态工业园区创建的现有条件

生态工业园是根据循环经济理念和工业生态学原理而设计建立的一种新型工业组织形态,在园区内通过废物交换、循环利用、清洁生产等手段,实现资源利用的最大化和废物排放的最小化.文章通过对大庆市石油、石油化工产业链现状分析及产品代谢和废物代谢分析,说明大庆红岗具有创建生态工业园区的区位和资源优势,园区所在区域内现已经初步形成了石油开采、石油化工、轻烃加工和化工建材产业(品)代谢连及废油、废水回注等废物代谢链的生态工业雏形,为创建大庆红岗生态工业(石化)示范园区奠定了一定的基础.     

试论煤矿区生态环境保护的措施与对策

对煤矿区开发建设中存在的主要生态问题，提出了相应的技术保护措施及其管理对策。     

上杭紫金山金矿废水废渣的处理及生态环境影响

金矿的开采会产生大量的废渣和废矿石，氰化法提金则产生大量含氰废水，如果未能妥善处理，将严重污染地表水和地下水，以及周边生态环境。该文对上杭紫金山金矿的生产工艺、废水废渣处理情况进行了调研，并提出矿山生态环境保护措施建议。     

北武夷下汪家铜多金属矿床地质特征及成因分析

下汪家铜多金属矿床形成于燕山晚期，成矿流体主要来自岩浆期后热液，断裂和岩浆岩是两大重要的成矿条件。控矿构造为北北东向断裂。成矿流体和主要矿质均源于地球深部，以上地幔或壳幔混合带为主，与燕山晚期富碱岩浆活动密切相关。下汪家铜多金属矿床成因上的分析，对该区下一步的找矿工作具有指导意义。     

利用微生物进行煤炭脱硫

从松藻煤矿分离到的氧化亚铁硫杆菌(Thiobacillus ferrooxidans)菌株T-4,能够利用煤炭中的黄铁矿作为能源基质,用含有细胞量10~8-10~9个/ml,pH1.55-1.70的种菌液,脱除煤炭中的无机硫,并进行了细菌煤炭脱硫的条件试验,9个样品4—72h试验结果,总硫量由1.31—2.45％降至1.05—1.88％,黄铁矿硫脱除率达86.11—95.16％.     

Characterisation of Organic Matter and Carbon Cycling in Rehabilitated Lignite-rich Mine Soils

Open-cast lignite mining in the Lusatian mining district resulted in rehabilitated mine soils containing up to four organic matter types: (1) recent plant litter, (2) lignite deposited by mining activity, (3) carbonaceous ash particles deposited during amelioration of the lignite-containing parent substrate and (4) airborne carbonaceous particles deposited during contamination. The influence of lignite-derived carbon types on the organic matter development and their role in the soil carbon cycle was unknown. This paper presents the findings obtained during a six year project concerning the impact of lignite on soil organic matter composition and the biogeochemical functioning of the ecosystem. The organic matter development after rehabilitation was followed in a chronosequence of rehabilitated mine soils afforested in 1966, 1981 and 1987. A differentiation of the organic matter types and an evaluation of their role within the ecosystem was achieved by the use of ¹⁴C activity measurements, ¹³C CPMAS NMR spectroscopy and wet chemical analysis of plant litter compounds. The results showed that the amount and degree of decomposition of the recent organic matter derived from plant material of the 30 year old mine soil was similar to natural uncontaminated forest soil which suggests complete rehabilitation of the ecosystem. The decomposition and humification processes were not influenced by the presence of lignite. On the other hand it was shown that lignite, which was thought to be recalcitrant because of its chemical structure, was part of the carbon cycle in these soils. This demonstrates the need to elucidate further the stabilisation mechanisms of organic matter in soils.