基于“3S”技术的辽宁省某尾矿库扩容工程生态影响预测与评价

以辽宁省某尾矿库为例,基于GIS技术,利用2010年的TM遥感影像及地形图,预测该尾矿库扩容后的生态影响。分析结果显示:尾矿库扩容工程对生态的影响主要体现在土地利用、植被、生态景观和地形地貌的变化4个方面。     

新疆恒源煤矿新近系水体采动等级评价

指出了恒源煤矿侏罗系煤系地层基本无水,主要充水水源为新近系独山子组的孔隙-裂隙含水层,但是主井筒开拓时,开始涌水量很小,继续向下开拓时,井筒涌水量超过1000m3/h。计算了煤层"两带"高度和新近系含水层与下覆煤系地层间距,研究表明:煤系地层与新近系水体间并无直接的水力联系,具体的涌水来源尚无定论,估算矿井的最大涌水量为160.74m3/h,正常涌水量为53.58m3/h。     

干旱矿区不同干扰强度下土壤种子库特征

土壤种子库是矿区植被恢复的重要因素,其特征在一定程度上反映了区域的植被恢复潜力。本研究通过样地调查和室内萌发法对乌海新星煤矿区3种不同干扰条件下的土壤种子库及与其地表植被之间的关系进行分析。结果表明:1)新星矿区土壤种子库共有18种植物,隶属于7科16属,物种生活型以多年生草本植物为主;2)新星矿区土壤种子库平均储量较小(226.51~739.17粒·m^?2),并且随着土层深度增加而呈递减趋势,其90%以上的种子储藏在0?10 cm的表层土壤;3)研究区土壤种子库植物与地上植被的共有物种数少,土壤种子库与地上植被的植物群落相似性较低;4)随着干扰强度的增大,种子库的植被恢复潜力呈现先增大后减少的趋势:道路周边受到中度干扰的自然植被区朝着有利的方向发展,而采矿周边受重度干扰的自然植被区会受到较大负面影响,其多样性以及与其他分区植物群落的相似性较小,种子密度显著降低(P<0.05)。     

基于物联网的矿山安全系统

文章分析总结了当前数字矿山中物联网的矿山安全现状,提出一种固定感知与移动感知相结合,孤立感知与联合感知相结合的矿山安全系统方案,简要分析了该方案的科学性和可行性。     

Using the RUSLE to identify factors controlling erosion rates of mine soils

Observable differences in particle size, smoothness and compaction between cap site (slope 2·8 per cent) and batter site (slope 20·7 per cent) surfaces on the waste rock dump at Ranger Uranium Mine were quantified in terms of revised universal soil loss equation (RUSLE) parameter values. Cap site surface material had a K_m (erodibility corrected for sediment density) of 0·030 and batter site surface material had a K_m of 0·0056. Using these K_m values (derived from particle size distributions), slope length and steepness (LS) factors of 0·36 for the cap site and 3·66 for the batter site, and a cover (C) factor of 0·45 for the cap site and 0·16 for the batter site, the RUSLE predicts an erosion rate from the cap site that is 1·9 times greater than erosion from the much steeper batter site. The RUSLE indicates that the finer particle size and blocky soil structure of the cap site (D₅₀ = 0·91 mm) compared with the looser granular structure of the batter site (D₅₀ = 1·74 mm) strongly influence erosion. The predictions are similar to observed soil losses from erosion plots on these sites under rainfall simulation events, for which the measured erosion rate from the cap site was approximately twice that from the batter site. For the RUSLE to predict the observed erosion rates, the support practice (P) factor for the cap site would have to be approximately 30 per cent greater than the P factor for the batter site. The higher cap site P factor probably results from smoothing and compaction caused by vehicle movement across the surface. Compaction is considered to have greatly reduced infiltration capacity, thus increasing the erodibility of the cap site. Vehicles probably also crushed the surface material at the cap site, creating the observed finer particle size distribution and further increasing the erodibility. Compaction, through its effects on erodibility (K_m) and surface roughness (P), is concluded to be the major cause of higher erosion from the cap site, even though the slope steepness is 10 times less. Parameterisation of the RUSLE quantifies the differences between sites and explains the unexpected erosion rates observed. The results highlight the need for careful management of rehabilitated sites to avoid increases in erosion which may arise from compaction by machinery.     

Metal contamination from open-cast copper and sulphur mining in southeast Ireland

The metal content was determined in soil and vegetation around the eastern zone of the disused sulphur and copper mines at Avoca (southeast Ireland). A 250 m × 250 m grid survey was conducted covering a total area of 4 km². The mining belt was in the centre of the investigated site and was sampled separately. Iron, Zn, Cu and Cd concentrations in soil and plant material were determined, in addition to soil organic matter content and soil pH. Soil samples taken from the spoil showed elevated Cu and Cd concentrations, and low soil pH and organic matter content. At least 50 per cent of the agricultural sites examined around the East Avoca Mine showed elevated soil Cu and Cd concentrations, whereas Zn and Fe soil concentrations were within the range for unpolluted soils. None of the vegetation analysed had elevated Zn, Cd, Fe or Cu concentrations. Overall there was no indication of serious metal contamination in either soils or vegetation surrounding the mine in spite of extensive dust deposition during open-pit mining activity 15–30 years ago. However, a plume of elevated Cu in the soil was identified, which originated from a large spoil heap and had been spread for some 2·0 km by the prevailing wind.     

南丰、衢州产区土壤及叶片中铜、锰含量的状况分析

采取南丰75个和衢州41个柑橘园土壤及叶片,对样品中铜和锰的含量进行分析。结果表明：南丰和衢州柑橘园土壤有效铜均表现为过量。其中,南丰土壤有效铜平均含量为3.00mg/kg,铜过量比例为85.3%;衢州土壤有效铜含量平均为3.68 mg/kg,铜过量比例为95.1%。南丰柑橘园土壤有效锰含量平均为7.41 mg/kg,缺乏比例为22.7%,适量比例为77.3%;衢州柑橘园土壤锰含量平均为7.21 mg/kg,缺乏比例为26.8%,适量比例为73.2%。南丰和衢州柑橘叶片铜含量均表现为过量。其中,南丰柑橘叶片铜含量平均为54.68mg/kg,过量比例为98.7%;衢州柑橘叶片铜含量平均为51.49mg/kg,过量比例为95.1%。南丰柑橘叶片锰含量平均为117.78 mg/kg,过量比例为78.7%;衢州柑橘叶片锰含量平均为99.79 mg/kg,过量比例仅为2.4%,其余均为适量。     

不同有机肥对矿区复垦土壤磷素矿化特征研究

【目的】探究不同有机肥对采煤塌陷复垦土壤磷素的矿化特征。【方法】采用室内培养试验,以不施肥处理为空白处理(CK),研究了施用3种有机肥(鸡粪、猪粪、牛粪)对矿区复垦土壤速效磷的动态变化,并综合其矿化过程中的磷酸酶活性及磷转化强度,分析了不同有机肥对矿区复垦土壤磷生物有效性的影响。【结果】①在整个室内恒温培养过程中,各施肥处理的速效磷量均随培养时间延长呈下降趋势,不同培养时期速效磷量大致呈现出:鸡粪>猪粪≥牛粪>化肥>CK。培养结束时(105d),鸡粪、猪粪和牛粪处理较化肥处理显著提高了土壤速效磷量(18.56%~37.09%);鸡粪处理较猪粪和牛粪处理速效磷量显著提高了11.93%~15.62%,而猪粪和牛粪处理间差异不显著;②在整个室内恒温培养过程中,拟二阶动力学模型能较好地反映各施肥处理速效磷释放过程,其次为Elovich模型和幂函数模型,而粒内扩散模型拟合效果较差。③在整个培养时期施有机肥处理的磷酸酶活性显著高于化肥处理,提高幅度为39.14%~120.70%。④培养前期(0~14 d),猪粪处理与化肥处理对土壤有机磷转化强度影响较大,二者间差异不显著,且猪粪处理较牛粪、鸡粪处理能显著提高有机磷转化强度,分别提高了41.51%和86.52%;在培养中后期(42~105d)各施肥处理的有机磷转化强度差异均不显著。【结论】施用有机肥能促进矿区复垦土壤磷素矿化,其中鸡粪较猪粪和牛粪对提高土壤有效磷量作用更为明显。     

杨庄煤矿区农田塌陷水域多介质OCPs污染特征及生态风险研究

为研究采煤活动影响下农田塌陷水域有机氯农药(OCPs)的污染特征及潜在生态风险,使用GC-MS对淮南潘一矿的杨庄农田塌陷区水体和底泥中的OCPs特征污染物六六六(HCHs)及滴滴涕(DDTs)进行质量浓度测定,利用ArcGIS进行OCPs分布特征及来源研究,并选择共识沉积物质量基准法(CB-SQGs)对潜在生态风险进行分析。结果表明:杨庄沉陷区溶解态ΣOCPs质量浓度范围为72.06～218.89 ng·L~(-1),均值为167.32 ng·L~(-1);悬浮态和沉积态ΣOCPs范围为199.35～405.04 ng·g~(-1)dw和24.34～1 247.32ng·g~(-1)dw,均值为277.07 ng·g~(-1)dw和238.78 ng·g~(-1)dw;悬浮态和沉积态OCPs质量浓度自上游向下游方向随水流呈削减趋势;杨庄塌陷水体中HCHs主要来自于林丹,DDTs主要来自于农业三氯杀螨醇;溶解态OCPs低于国家Ⅲ类水质标准限额,处于低生态风险水平;悬浮态和沉积态OCPs处于中高生态风险水平,其中沉积态OCPs毒性发生率略低于悬浮态OCPs毒性发生率。     

Geomorphic estimates of the stability of a uranium mill tailings containment cover: Nabarlek,Northern Territory,Australia

The geomorphic stability of the cover (cap) over the pit of Nabarlek Uranium Mine in Arnhem Land, Northern Australia, is important because radon gas and other long-lived radio-nuclides arising from mill tailings must be contained for long periods. The primary agents of denudation in the region's seasonally wet tropical environment of low relief are rainwash, overland flow, rilling and gullying. Other agents of erosion are of less concern, although biogenic agents of erosion (e.g. termites and windthrow) may enhance fluvial activity. A combination of modelling, using the Universal Soil Loss Equation, and analogue estimates of denudation and thresholds of rilling and gullying from areas with similar geology, topography and climate are used to estimate the stability of the Nabarlek cover. Denudation rates are conservatively estimated at less than 100mm ky⁻¹. It is suggested that with some minor design modifications the cover will retain its integrity for several thousand years.