Adaptations to the dynamics of rural water supply from natural sources: A village example in semi-arid Nigeria

Domestic and agro-economic activities in the semi-arid region of Nigeria rely exclusively on rainfall, streamflow and groundwater in deep and alluvial (fadama) aquifers. Such water supply systems are subject to considerable seasonal and inter-annual variability. However, a combination of the various sources may mitigate the effects of water scarcity. This study describes the dynamics of the water sources for a village in northeastern Nigeria as an example that demonstrates the linkages between rainfall, streamflow and groundwater. Such linkages are important for developing strategies to mitigate the effects of climatic variation. Long-term records of rainfall were not available at the site so that the short-term data was interpreted in the context of the long-term climatic experience of the region. The stratigraphic profile of the aquifer was developed from resistivity methods, to supplement information obtained from well level hydrographs. Field observations and analysis of the data reveal that the beginning of the rainy season is a precarious period because none of the water sources are reliable. Rainfall infiltration recharges the shallow aquifers while lateral water flux from the floodwater-saturated fadama also contributes to water level rises in the deep wells. A study of the water level changes in response to deepening of the wells suggests that the wells are fed by an assortment of water-bearing lenses, separated by layers of low transmissivity. One major finding of this study is that there exists a close association between the wells in this riparian community and the recharge processes within the fadama. Upstream diversion, abstraction or impoundment could therefore undermine the viability of aquifer exploitation by the communities in the riparian zone. Analysis of the interactions among the various sources of water leads to the identification of several potential adaptation strategies for confronting the problem of water scarcity.     

合肥台地电阻率干扰综述

本文首先叙述了合肥台地电阻率值ρS的观测环境,并根据合肥台近年几次ρS的异常变化,通过初步理论分析,找出了DD-1接地体、电缆沟开挖、大气降水、太阳黑子引起的自然电场对ρS的干扰,为以后排除和识别地电干扰起参考作用.     

大武口发电厂3号炉电除尘器改造

根据大武口发电厂3号炉飞灰比电阻高的特点，对电除尘器进行了改造，使除尘效率由原来的97．3％提高到99.5％。     

一种导电混凝土的制备及其电阻率测量

本文综述了导电混凝土的发展以及应用情况，提出了用导电混凝土作为接地材料的设想，并选择氧化铁粉作为骨料，添加适量碳粉配制了一种导电混凝土来验证。通过改变不同的配比制作导电混凝土模型，用四电极法测量其电阻率，得出碳粉比例对其电阻率的影响。     

LNAPL在砂质含水层中动态迁移的电阻率法监测试验研究

在海滨潮间带采集细砂,通过室内柴油泄漏模拟试验,利用自制电阻率监测系统对轻非水相液体在砂土-地下水系统垂向渗透过程进行电阻率变化动态监测;通过配制不同含油率砂土测定其静态电阻率变化规律,探讨电阻率变化的影响因素;最后取样分析测定污染含水介质稳定后含水率及含油率,对监测结果有效性进行了验证;并利用显微成像法对污染砂土进行了微观形态分析.结果表明,柴油污染砂土微观形态上胶结现象明显;柴油渗透海滨砂土过程电阻率大小同含水饱和度,比电阻率和含油饱和度之间存在良好的相关性,均可用Archie公式拟合,n值分别为2.36和0.15;通过电阻率测定可以有效估算柴油透镜体厚度;电阻率随深度的变化可以反映含油率和含水率的垂向分布.本研究为轻质油品储罐或者海上油品输运过程泄露造成的海滨砂土地下污染扩散过程监测及机制研究提供了一种有效的方法,也可为其他典型石油泄漏污染场地的电阻率法探测或监测提供参考.     

旋转电极式电除尘器技术研究

简要阐述了旋转电极式电除尘器的原理、结构、应用及特点,并总结出其除尘效率计算公式。研究结果表明：该技术能最大限度的减少二次扬尘,显著降低电除尘器出口排放浓度,对高比电阻粉尘有很好的收尘效果。与其他除尘器比较,旋转电极式电除尘器节省场地、空间和能源,性价比高,具有较广阔的应用前景。     

大型测控设备的接地系统设计与探讨

介绍了接地的目的和种类,针对大型测控设备对接地电阻值的要求,提出了区域面积受限的接地系统设计方案,并对接地电阻进行了详细分析、计算和比较,选出了合理的接地方案进行施工,竣工后对接地系统的接地电阻值进行检测,检测结果满足测控设备接地电阻的要求.     

安徽嘉山台的多极距电阻率观测

利用1990年以来安徽嘉山台的多极距电阻率观测资料进行反演分析，结果显示： 嘉山台的浅层(第一层)电阻率变化幅度最大，认为是受气象和灌溉等因素的干扰； 第二层变化幅度迅速减小； 第三层变化平稳； 深层(第四层)电阻率变化幅度比二、 三层大，可能与层厚为∝有关，原因尚须进一步研究。     

高邮地震台地电阻率观测精度干扰原因分析及排除方法

对高邮台地电NS向ρs的观测精度在2002 07 24雷雨后出现降低的现象进行了分析排查,发现是一交流接触器在遭雷击时烧坏,导致交流电三相中的一相对地漏电,与变压器中的零线形成回路所致。从而排除了配电房漏电的干扰,保证了观测资料的质量。     

DETECTION OF FRESH WATER AQUIFERS IN THE GLACIAL DEPOSITS OF NORTHWESTERN MISSOURI BY GEOELECTRICAL METHODS1

Geoelectrical investigations in Grundy County of northwestern Missouri, where the groundwater resources of the glacial deposits have already been examined through an extensive drilling program by the Missouri Geological Survey and Water Resources, indicate that water-bearing gravel deposits can be distinguished from glacial deposits containing appreciable amounts of clay and limited amounts of water. The Schlumberger method used for the geoelectric depth soundings in the vicinity of the Survey's drillholes demonstrates the exploratory usefulness of the method in that it can partly replace the more expensive procedure of drilling. The method also provides improved interpretation between drillholes. Results of the investigation show that, in the area, clay has a resistivity below 20in, that the fresh water-bearing gravel at the bottom of the buried glacial stream channels has a resisitivity of 40 to 50fim, and that the near surface glacial gravel deposits have a resistivity above lOOfim. Interpretation of the depth soundings and the conductivity of water obtained from a local well implies that its water is drawn from the saline water of the bedrock. A recommendation is made for the quality improvement of this particular well.