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Water security is related closely to ecological, environmental, economic, social, and political problems, and may possibly even affect national security. The problem is especially important in arid inland watersheds. In this paper, we assess the water resources security of three watersheds in the Hexi Corridor (Northwest China) using a multi-level, multi-target, analytical hierarchy process approach. We constructed an assessment system based on the current situation and future development of the region’s water resources in the context of the society, economy, and environment of these inland watersheds. The assessment used 21 indicators that describe the ratio of water supply to demand, the ecological environment, food security, drinking-water security, disaster control capacity, water resources management, and economic conditions. The level of the water resources security was highest in the Shulehe watershed, followed by the Heihe watershed and the Shiyanghe watershed. Strategies to promote water security for all three watersheds are discussed.

A significant component of domestic demand for water of urban areas located in the Gangetic plains is met by heavy pumping of groundwater. The present study is focused on the Patna municipal area, inhabited by 17 million people and spanning over 134 km2, where entire urban water demand is catered from pumping by wells of various capacities and designs. The present study examines the nature of the aquifer system within the urban area, the temporal changes in the water/piezometric level and the recharge mechanism of the deeper aquifers. The aquifer system is made up of medium-to-coarse unconsolidated sand, lying under a ~40-m-thick predominantly argillaceous unit holding 8- to 13-m-thick localised sand layers and continues up to 220 m below ground. Groundwater occurs under semi-confined condition, with transmissivity of aquifers in 5,500–9,200 m2 day−1 range. Hydraulic head of the deeper aquifer remains in 9–19 m range below ground, in contrast to 1–9 m range of that of the upper aquitard zone. The estimated annual groundwater extraction from the deeper aquifer is ~212.0 million m3, which has created a decline of 3.9 m in the piezometric level of the deeper aquifer during the past 30 years. Unregulated construction of deep tube wells with mushrooming of apartment culture may further exacerbate the problem. The sand layers within the aquitard zone are experiencing an annual extraction of 14.5 million m3 and have exhibited stable water level trend for past one and half decades. This unit is recharged from monsoon rainfall, besides contribution from water supply pipe line leakage and seepage from unlined storm water drains.

The Afyon Castle is a tourist destination and a historical site in the City of Afyon in Turkey. The Castle is located on a steep hill, with a height of 226 m. In close proximity to the Castle there are settlements. The hill consists of trachitic andesite. The rock contains columnar joints and flow layering. Owing to these discontinuities, blocks of varying sizes had fallen down. The settlement areas near the Castle are now in danger because of the rockfall risk. In this study, rockfall analysis was carried out along nine profiles of the hill. Fall-out distance, bounce height, kinetic energy and velocity of the rocks along each profile were investigated. The results of the analyses were evaluated, and the areas delineated as susceptible to rockfall risk are highlighted. Remedial measures including rock bolts and protective fences were suggested on the basis of the field observations and the rockfall risk evaluation.

With the large-scale application of nitrogen fertilizers in the agricultural area, the karst area in southwest China is increasingly polluted by nitrogen. Understanding the distribution, transportation, and sources of nitrogen is the premise for effective pollution control in the catchment. The present study used the nitrogen and oxygen isotopes technique to explore the dynamic changes and sources of nitrates during rainfall in various land uses in a typical karst catchment in southwestern China. The results of hydrochemistry composition indicated that agricultural activities have caused the deterioration of water quality, while intensive rainfall during the wet season has played a positive role in promoting it. NO3−–N was the major inorganic N, accounting for 78.7 ± 21.6% (N = 38) of the total nitrogen. Dryland and paddy field provided a large amount of nitrogen for the water environment by rain, which contributed to high NO3−-N concentration in spring (6.1 ± 0.9 mg/L) and runoff (7.2 ± 0.9 mg/L) at the catchment outlet. Nitrate isotopic compositions (δ15N–NO3− and δ18O–NO3−) and water isotopes (δD and δ18O–H2O) revealed that isotopic composition in dryland and paddy field was mainly affected by nitrification. Source analysis showed that dryland and paddy field was dominated by chemical fertilizers and manure, while precipitation and soil organic nitrogen were the major sources in abandoned land, forest and shrub. This study highlighted that land management and nitrogen fertilizer application should be reasonable to reduce the risk of nitrogen surplus in the water environment.

The mineralogy and geochemistry of the waste rocks distributed at Taojiang Mn-ore deposit, central Hunan province, China, were studied using X-ray powder diffraction (XRD), electron microprobe analysis (EMPA) fitted with energy dispersive spectrometer (EDS) and inductively coupled plasma mass spectrum (atomic emission spectra) ICP-MS (AES), with the aim of predicting the environmental impacts of weathering of the waste rocks. The mineralogical results from microscope observation and XRD and EMPA studies show that the waste rock is composed of black shale and minor Mn carbonates. The oxidation of sulfide minerals such as galena, pyrite and chalcopyrite is accompanied by decomposition of Mn carbonates and K-feldspar during exposure to atmospheric O2. The geochemical characteristics of major, rare earth elements (REE) and trace elements of the waste rocks also show that the waste rock can be divided into black shale and Mn carbonate, and both of them are currently under chemical weathering. The major alkalies and alkaline elements (Ca, Mg, Na, K, Rb, Sr and Cs) and major elements (Fe, S and P) and heavy metals (Sc, V, Cr, Th, U, Sn, Co, Ni, Cu, Zn, Pb, Mo, Cd, Sb, an Tl) are being released during weathering. The mobility of alkalis and alkaline elements Ca, Mg, Na, K, Rb, Sr and Cs is controlled by decomposition of Mn carbonates. The dispersion of Cr, Sc and Th (U) might be related to weathering of K-feldspar, and the release of the heavy metals Co, Ni, Cu, Zn, Pb, Mo, Cd Sb and Tl is dominated by the breaking of sulfide minerals. The REE of the waste rocks and surrounding soils and the spidery distribution patterns of heavy metals in the waste rocks, the surrounding soils and the surface waters show that weathering of the waste rocks and bedrock might be the sources of heavy metal contamination for the surrounding soils and surface water system for the mining area. This is predicted by the mass-balance calculation by using Zr as an immobile element. Therefore, it is urgently necessary take measures to treat the waste rocks distributed throughout the area for the local environmental protection.

The aim of this article is twofold. Firstly, the water quality of the Lower Danube River is assessed using the data collected at three points at Chiciu km 375 (in Romania), during the period January 2010–December 2012 by computing the CCME Water Quality Index. Secondly, a similarity study for 17 series of water parameters recorded at the study sites is performed. CCME Water Quality Index, yearly computed, varied from Fair to Good, with an overall rating as Fair. Some dissimilarities of chemical oxygen demand, biochemical oxygen demand, N-NO4, N-total, Cu, Ni distributions are noticed.

The coastal region of Southern Italy’s Caserta province, known as the Litorale Domitio (Domitia coast) has been subjected to increasing pressure from unsustainably fast economic and urban growth in the last century, that resulted in a induced serious land degradation. To obtain a comprehensive picture of the ecological status of the Domitia coastal zone (Campania, Southern Italy), a holistic methodology has been applied. Sedimentological, geochemical, and biological analyses of the surface sediments and water samples were performed along the submerged beach. The data were integrated using a geographical information system, together with information on past and present land use and human activities along the coast and in inland regions. Heavy metal concentrations in sediments plus As and Se (Cd, Co, Cr, Cu, Hg, Ni, Pb, V, Zn) and their enrichment factors, which are important for identifying polluted areas in countries like Italy (where environmental legislation has not yet established intervention limits), indicate excesses Cd, Cr, Pb, and V of probable anthropogenic origin. A microbiological contamination of marine waters has been detected by the Regional Environmental Protection Agency of Campania. The Bacteriological Quality Index map shows that bathing areas must be classified as “contaminated” and “highly contaminated”. High levels of chemical and biological contamination are particularly common in both bathing seawater and sediments along the coastal zone south of the Volturno River, where the existing wastewater treatment plant is not properly working, to date. Factory farming, which is widespread in the area, is likely to be an additional important source of contamination. In accordance with these conclusions, analyses of the benthic diatom community revealed dominance of eutrophic species.