Conflicting drainage patterns in the Matera Horst Area,southern Italy

The Matera Horst (“Murgia materana”) is included in the Apulian plateau, basically formed by Mesozoic shallow-water carbonates. The zone is located in a present-day temperate belt and form a flat-topped morphostructural large element inside the foreland area of the southern Apennines. This horst is bordered by high-angle faults and surrounded by downthrown blocks covered by Plio-Quaternary marine and alluvial sediments. The structural high experienced several morphological cycles from Miocene to Quaternary. In particular, three evolutionary stages can be recognized at least. The first stage is currently represented by relics of a flat erosional landscape at the top of the relieves. The second one is testified by gentle slopes with wide glacis at the foothills, locally covered by coarse waste deposits. During the third stage a series of marine terraces formed and a drainage system developed creating both bland valleys and well-defined channels and gorges. The latter streams deeply carve the Cretaceous limestone of the Matera Horst for they represent the morphological response to the tectonic uplift of the area and clearly post-date the former features. Since the fluvial net took place on Pleistocene covers, later widely eroded, it is possible to conclude that the major part of the Matera Horst drainage system represents a good example of superimposition. However, low order streams and segments of major rivers appear to be structurally controlled, as suggested by comparison with the fracture system. Further, also open synclines and gently steeped flexures may locally exert a driving control on minor streams. These apparently conflicting genetic hypotheses can be explained by the role of exhumation of inherited structures of the bedrock in add to a constant interplay between tectonics, erosion and drainage evolution during Quaternary times.     

煤电钻技术在探放老空水中的应用

通过 对采 空区 积 水规 律的 分 析与 研究 ,提 出在 积 水采 空区 下 沿空 掘进 采 用煤 电钻 探 放水 技术 及 方法 ,解 决了钻 机探 放 水的 塌孔 问 题,既保 证了 沿 空掘 进的 安 全,又 取 得了 较大 的 经济 效益 。     

Combination of drainage, water supply and environmental protection as well as rational distribution of water resource in Zhengzhou mining district

It is forecasted that before the 2050s, coal would still make up 50%-60% of once energy constitution in China, but unfortunately, in most part of our coal districts and peripheral regions, we generally face the contradiction and conflict among the threat of water hazard, shortage of water resource and environmental protection, which are becoming more and more serious especially with a gradual increase in mining depth of the shaft and recovery of lower coal beds. The concrete expression is as f…     

Temporal variation in discharge chemistry and portal flow from the 8-Level adit, Lynx Mine, Myra Falls Operations, Vancouver Island, British Columbia

The Lynx mine, currently inactive, has produced copper and zinc concentrates from massive sulfide deposits on a lease within the rainy, mountainous interior of Vancouver Island. Tailings, used to back-fill a mined-out stope, are being leached by percolating groundwater and the resulting acidic, metal-laden drainage is discharging from the portal of the 8-Level adit. Temporal variations in the flow rate, specific conductance and temperature of the discharge were monitored continuously over a 2-year period while effluent chemistry was sampled weekly. Conductivity was relatively constant throughout most of the year but peaked with the first autumn storm events as accumulated soluble sulfide oxidation products were flushed from the workings. Concentrations of sulfate and most metals were closely correlated with conductivity as were low pH values as stored acidity was released along with dissolved species. Variations in pH controlled the speciation and partitioning of metals between dissolved and particulate phases.     

多面聚能射孔压裂排放瓦斯的研究

复合射孔技术能有效地控制射孔方向和压裂缝的扩展。对其作用机理进行了初步的分析研究 ,并对相关参数进行了理论计算。针对煤层的特性 ,将该技术用于煤层致裂 ,经过现场应用 ,效果良好。该技术在煤层致裂爆破中的发展方向较多 ,有良好的应用前景     

在我国发现的Schwertmannite矿物及其特征

采用X射线衍射(XRD)、扫描电镜与能谱(SEM-EDX)、X射线荧光(XRF)、傅立叶红外光谱(FT-IR)、热分析(DTA-TG)等分析方法,在我国山西马兰煤矿的酸性矿坑排水(AMD)沉淀物中首次发现了“斯沃特曼铁矿”(Schwertmannite)。研究表明,山西马兰煤矿酸性矿坑排水沉淀物中的Schwertmannite矿物的粒径为0.3~70μm,且分布比较均匀,其BET表面积为44.065 0 m2/g;SEM二次电子像显示为球形或椭圆形(聚集体)结构,颗粒大小比较均匀,球的表面有针状毛刺;该矿物的化学式为Fe8O8(OH)4.52(SO4)1.74.4.73H2O。     

Barium anomaly in Kupa River drainage basin

The objective of this work is to present an example of environmental impact of barite waste management observed in stream sediments of the western part of the Kupa River drainage basin. It is a significant water resource for Croatia and a part of Slovenia. In addition, it is for both countries a region of tourism, sport and fishing. Sediments (fraction < 63 μm) collected within the whole drainage basin have shown a significant barium anomaly in the western part. The highest concentration of total barium (5790 mg/kg) was determined in Kupica, a tributary of Kupa River. The barium anomaly was traced in Kupa River about 120 km downstream. Looking for the contamination source it was found that the anomaly originates from uncareful waste disposal into an abyss, after barite separation in Homer (Lokve), Gorski Kotar, Croatia. From there barite entered Kupica River subterraneous. Barite and albite were identified by XRD near the source of Kupica River as minor minerals, while quartz and dolomite ferroan were major minerals. This preliminary report does not give yet an answer about barium solubility in river water, about its bioavailability and consequently about barium pollution in the western part of the Kupa River drainage basin, however the possibility is highlighted and discussed.     

淮北煤田矿井充水因素与防治水措施研究

淮北矿区矿井突水的主要充水水源是老窑积水、新生界松散层底部含水层（组）水、煤层顶、底板砂岩裂隙水、太原组与奥陶系灰岩水。矿井众多重大突水事故表明，加强太原组、奥陶系石灰岩含水层和断层破碎带的探测与疏放工作，是降低煤矿突水风险的必要条件。     

长江流域各地区环境保护水平分析

长江流域总面积180×104km2,约占全国总面积的18.75%,跨越了东中西三大经济地带,联接了南北地方经济。在长江流域发展的历史过程中,除了社会进步与经济增长之外,也是中国环境污染较严重的地区之一。根据因子分析方法与原理,选择一系列指标,并将其归结为条件因子和治理因子,在此基础上对长江流域的环境保护水平进行了综合评价,分析了流域内各个地区之间存在的具体差异,指出对环境保护事业的高投入是环境保护水平提高的必要而非充分条件,而且各地区根据经济和污染状况的差异,应该采取不同的改进策略。     

桐柏—大别山掀斜隆升对长江中游环境的影响

桐柏－大别山自早更新世晚期以来,不断发生着自北向南的掀斜隆升,从而对长江中游的环境,尤其是水系的演化产生了严重影响。主要表现在：鄂西各东西向河流的阶地高差自北向南逐渐降低;江汉平原水系同步向南发生异常弯曲,长江主河道不断南移,湖相沉积范围也由北向南收缩和迁移;鄂东长江两岸水系和河谷地貌发育不对称,长江主河道紧逼南岸丘陵区。现代地壳形变资料表明：桐柏－大别山的掀升作用仍在继续,由此引起的环境问题还将