延长大型露天矿铁路运输服务年限的浅见

大型露天矿在由山坡型转入深凹型开采后,随着运输条件的恶化,将单一的准轨铁路运输,改变为铁路—汽车联合运输,以延长铁路运输的服务年限,为此,需要解决提高电力机车运输性能、改造运输线路系统等问题。     

矿用丁腈橡胶覆盖胶橡塑整芯输送带的粘合研究

概述矿用丁腈橡胶覆盖胶橡塑整芯输送带研制的意义。通过丁腈橡胶覆盖胶配方设计试验体会，对影响盖胶与带芯粘合的丁腈橡胶类型、增塑剂品种的选择及共硫化、混炼胶的停放等因素进行讨论。     

Upscaling hydraulic conductivity: theory and examples from geohydrological studies

This paper presents an overview of the theory of upscaling hydraulic conductivity and describes two case studies in which some of this theory has been applied. The representative hydraulic conductivity of a numerical model block (block conductivity for short) is defined in terms of smaller scale hydraulic conductivities. Also, using elementary examples, some general properties of block conductivities are given. Analytical solutions for the block conductivity are presented that were derived by various authors for uniform flow conditions both in a deterministic and in a stochastic setting. Some results of the hydraulic upscaling theory are illustrated by two case studies from the Netherlands. The first case study deals with deriving the representative hydraulic conductivity tensor of a clay layer. Upscaling results are compared with traditional harmonic averaging. In the second case study the upscaling is used to derive the three-dimensional distribution of block conductivities for a numerical groundwater model of a confining layer of complex deposits. Here stochastic upscaling is used together with a geostatistical simulation approach. The simulated block conductivities are used in a numerical groundwater model and results are compared with pumping tests. When the upscaling is ignored groundwater flow through the deposits is predicted wrongly.     

Has water-saving irrigation recovered groundwater in the Hebei Province plains of China?

This study performed a quantitative evaluation of the impact of water-saving irrigation on the groundwater regime in the Hebei Province plains area. In this work, the change in groundwater regime and the contributions of precipitation and water-saving irrigation development were investigated. The results indicate that the groundwater overdraft has been mitigated to some extent, mainly due to changes in precipitation and the implementation of water-saving irrigation, with contributions of 64.3% and 35.7%, respectively, when considering only these two factors. Water-saving irrigation is accepted as an important means for reducing groundwater depletion, but should be used in conjunction with other measures.     

长大隧洞工程建设中地下水处理的实践及思考

以引汉济渭工程秦岭输水隧洞(越岭段81.779 km)为例,围绕该隧洞建设过程中的地下水问题,介绍其总体富水情况以及地下水预测方法。通过对秦岭各支洞抽排水措施的综合研究,给出了抽排水方案的设计步骤,结合不同涌水的处理提出了突涌水的处理思路,并介绍了目前国内先进的突涌水预测手段及应用效果。根据秦岭隧洞抽排设备的配置思路以及洞外环保处理情况,指出了目前地下水处理过程中存在的问题并提出相应的解决方法。通过引汉济渭工程建设过程中地下水处理情况的介绍、探讨和分析,对长大隧洞处理类似地下水问题提供一定的借鉴。     

华北平原地下水资源承载力评价

华北平原地下水严重超采,并带来一系列资源环境问题,地下水资源承载力的可持续性面临严重挑战。本研究定义了地下水资源承载力的概念,提出了一种定量评价地下水承载力的新方法,并对华北平原地下水承载力进行了评价。结果表明,华北平原地区地下水资源支撑的GDP从2003年的15 608.18亿元迅速提高到2011年的37 584.9亿元,33.3%的地市位于未超采未超载区;华北平原整体及57.2%的地市均位于超采未超载区,已发生地下水超采,但通过提高用水效率,未来社会经济规模仍有发展空间;9.5%的地市位于超采超载区。最后探讨地下水资源的承载力的提高途径,主要包括增加地下水资源可利用量和提高用水效率两方面,其中提高用水效率效果更显著。     

陈家冲垃圾填埋场地下水环境健康风险评价

垃圾填埋是目前国内处理城市生活垃圾的主要方式,由垃圾渗滤液引发地下水环境污染已成为当前主要的水环境问题之一。选择武汉市陈家冲垃圾填埋场为研究对象,通过对该区周边地下水布孔取样和监测,分析了垃圾填埋场对其周围地下水环境的影响。结果表明:研究区地下水的主要污染因子为Pb、Cd和Fe,且各污染物的浓度与采样深度、井距呈负相关关系。垃圾填埋场产生污染的影响范围主要在距离800m以内、深度小于5.5m的地下水。为进一步了解该区地下水对人体健康危害的风险程度,对研究区地下水进行了水环境健康风险评价,结果显示:研究区各采样井地下水的总风险值在2.71×10~(-4)/a~7.12×10~(-3)/a,均超过国际辐射防护委员会(ICRP)推荐的最大可接受值5.0×10~(-5)/a,主要风险因子为基因毒物质Cd和Cr(VI)以及躯体毒物质硝态氮;其中,Cd和硝态氮所致的健康风险值超标率100%,而Cr(VI)的健康风险值超标率为50%,对暴露人群存在健康危害风险。此外,对男性和女性健康风险值的研究显示,研究区地下水环境中污染物的男性健康危害风险值普遍高于女性。     

北京地面沉降与地下水开采时空演变对比

区域地面沉降是世界上很多城市都要面对的一种"城市病"。地下水过量开采是这一问题最普遍的原因,北京也因此出现了严重的地面沉降问题。为了全面认识地下水开采格局变化下的地面沉降发育分布的新特点,推动实现《北京地面沉降防治规划(2013-2020年)》中的"控沉目标",对北京市从解放初期至今60多年间的地下水开采和地面沉降演变进行了时间和空间上的定性定量对比分析。结果表明:地面沉降的形成发展阶段与地下水开发利用阶段高度吻合;地面沉降中心区与地下水位降落漏斗区的时空变化高度相关;随着地下水开采深度整体上向地表以下更深层发展,主沉降层逐渐向深部(100m以下)地层转移,为地面沉降防控决策制定提供了依据。     

我国结构抗浮水位研究现状与展望

目前我国结构抗浮水位方面研究成果虽然很丰富, 但分歧很大, 不仅直接影响了实际工程中的应用, 同时也造成了研究工作自身缺乏系统性和延续性。为解决这一问题, 利用水文学、水力学和土力学等科学理论, 分别从抗浮水位基本概念、抗浮水位分析中两个基本问题(孔隙水压力和远期最高水位)的方法论和抗浮水位分析的技术体系等3个角度对既有研究成果进行了系统综述与客观分析。在抗浮水位基本概念方面, 根据地下水赋存和渗流理论, 将目前研究成果划分为二维、准三维和三维等3种类型, 提出了各自的数学表达式, 分析了三者之间逻辑关系, 讨论了各自的科学性和适用性。在孔隙水压力分析方法方面, 尤其是孔隙水压力折减问题, 对基于渗流理论和有效应力原理的经典分析方法进行系统评述的同时, 还对当前讨论热烈的基于结合水理论的分析方法进行了梳理评价。在地下水远期最高水位预测方面, 着重讨论了历史最高水位法、基于宏观数据反演法和数值分析法等3种方法的优缺点及需要完善之处。在抗浮水位分析技术体系方面, 以北京地区为例对该类问题作了简要总结与评述。最后, 对抗浮水位研究与应用现状进行了概要性评述, 并结合我国国情, 对未来工作提出了展望与建议。     

Chemical and Isotopic Tracer Evaluation of Water Mixing and Evaporation in a Dammed Texas River During Drought

The interaction between drought and river regulation is monitored to better understand river flow mixing, evaporation and surface‐groundwater exchange in changing regional climates and in increasingly regulated waterways. This study compared Brazos River stable isotope (δ¹⁸O and δD) and electrical conductivity values with reservoir, creek and aquifer samples in the Brazos watershed, the largest watershed in Texas. The combination of tributaries, rainfall and the Brazos River Alluvium Aquifer, on the one hand, and the Lake Whitney reservoir, on the other hand, represent endmembers of dilute run‐off water and evaporated saline water, respectively. A simple isotope mixing model that uses monthly river discharge, Lake Whitney discharge, historical monthly precipitation δ¹⁸O and pan evaporation accurately reconstructs river δ¹⁸O (±0.5‰ on average). Data and isotope balance modelling support continued evaporation of ¹⁸O‐enriched Lake Whitney water as it flows downstream, although the most evaporation took place in Lake Whitney. The difference between river and precipitation δ¹⁸O, or Δ¹⁸O_RIV‐_PPT, here a measurement of degree of evaporation, ranged from ?0.1‰ for a small creek, to 1.7‰ for the Brazos River, to at least 2.7‰ in Lake Whitney. This study indicates that drought in regulated rivers may enhance reservoir discharge dominance in river flows during peak drought conditions when combined run‐off and baseflow dominance would be expected in a similar undammed river. Copyright © 2016 John Wiley & Sons, Ltd.