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Dongmei Han Xing Liang Menggui Jin Matthew J. Currell Ying Han Xianfang Song 《Environmental management》2009,44(2):243-255
Based on analysis of groundwater hydrochemical and isotopic indicators, this article aims to identify the groundwater flow
systems in the Yangwu River alluvial fan, in the Xinzhou Basin, China. Groundwater δ2H and δ18O values indicate that the origin of groundwater is mainly from precipitation, with local evaporative influence. d-excess values lower than 10% in most groundwaters suggest a cold climate during recharge in the area. Major ion chemistry,
including rCa/rMg and rNa/rCl ratios, show that groundwater salinization is probably dominated by water–rock interaction (e.g.,
silicate mineral weathering, dissolution of calcite and dolomite and cation exchange) in the Yangwu River alluvial fan, and
locally by intensive evapotranspiration in the Hutuo River valley. Cl and Sr concentrations follow an increasing trend in
shallow groundwater affected by evaporation, and a decreasing trend in deep groundwater. 87Sr/86Sr ratios reflect the variety of lithologies encountered during throughflow. The groundwater flow systems (GFS) of the Yangwu
River alluvial fan include local and intermediate flow systems. Hydrogeochemical modeling results, simulated using PHREEQC,
reveal water–rock interaction processes along different flow paths. This modeling method is more effective for characterizing
flow paths in the intermediate system than in the local system. Artificial exploitation on groundwater in the alluvial fan
enhances mixing between different groundwater flow systems. 相似文献
2.
Hypsographs are graphic depictions of the vertical distributions of volumes or masses of water in lakes, ponds, or reservoirs. Quantitative limnological science or engineering must use a hypsograph, or a more complex equivalent system, to undertake calculations of water constituent concentration data by mathematical weighting. Construction of the graph is simple and described. Exemplary uses of the hypsograph are presented. 相似文献
3.
Inamdar S 《Environmental monitoring and assessment》2007,133(1-3):347-363
Storm event exports of dissolved were explored for multiple events in the Point Peter Brook watershed (PPBW), a glaciated, forested watershed located in Western
New York, USA. Investigations were performed across four catchments (1.6–696 ha) with varying topography and the extent of
surface-saturated areas. While wetland and riparian waters were important sources of during non-storm periods, throughfall and litter leachate were the dominant contributors of during storm events. Ammonium concentrations in catchment discharge displayed a sinusoidal seasonal pattern with a maximum
during early spring (March) and a minimum in late summer (August–September). Storm event concentrations of in streamflow were much greater than baseflow values and showed a consistent temporal pattern with an increase in concentrations
on the hydrograph rising limb, a peak at or before the discharge peak, followed by a decline in concentrations. Storm event
patterns of DON were similar to while the patterns of differed from for the summer and fall events. The storm event expression of was attributed to throughfall and throughfall-mediated leaching of the litter layer. The reactive behavior of precluded its use in an end member mixing model (EMMA) for predicting streamflow concentrations. While concentrations of
in precipitation and streamflow were high for the spring events, exports of in streamflow were highest for the large and intense storm events. Baseflow concentrations increased with the percent wetland/saturated area in the catchment but the same trend did not hold for storm-event
concentrations. 相似文献
4.
B. De Martis M. A. de Miranda Restivo A. Mocci Demartis E. Serra 《Environmental management》1992,16(3):381-388
Capoterra Pond in southern Sardinia is described and analyzed with respect to its morphological, meteorological, physical
and chemical characteristics, and its zoobenthic, zooplankton, and phytoplankton biocenoses. The birdlife, flora, and riparian
associations of vegetation are studied in order to draw international attention to the importance of this lagoon, the precariousness
of its ecosystem, the seriousness of current attempts to destabilize it, and the need to encourage the Sardinian authorities
to initiate conservation measures, especially as rare birds have found their niches there. 相似文献
5.
Sulfate () concentrations and fluxes were studied for multiple storm events in the Point Peter Brook watershed, a glaciated, forested
watershed located in Western New York, USA. Investigations were performed across one large (696 ha) and three small (1.6–3.4 ha)
catchments with varying extent of riparian and wetland areas. Concentrations of in groundwater sources (mean values: 238–910 μmolc L−1) were considerably greater than concentrations recorded for rainfall (60 μmolc L−1) and throughfall (72–129 μmolc L−1). Seasonality in concentrations was most pronounced for valley-bottom riparian waters with maximum concentrations in late winter–spring (February–March)
and a minimum in late summer (August). Concentrations of in wetland water were considerably less than riparian water indicating the likelihood of reduction in anoxic wetland conditions. Storm events displayed a dilution pattern in concentrations with a minimum coinciding with the maximum in throughfall contributions. End member mixing analysis (EMMA)
was able to predict the storm event concentrations of for four of the six comparisons. Concentrations of at the outlet of the large (696 ha) catchment were much greater than values recorded for the smaller catchments. Exports
of in streamflow exceeded the inputs from atmospheric deposition suggesting that watersheds like Point Peter Brook may not show
any immediate response to decreases in atmospheric deposition. 相似文献
6.
Kyoung-Ho Kim Seong-Taek Yun Byoung-Young Choi Gi-Tak Chae Yongsung Joo Kangjoo Kim Hyoung-Soo Kim 《Journal of contaminant hydrology》2009,107(3-4):114-127
Hydrochemical and multivariate statistical interpretations of 16 physicochemical parameters of 45 groundwater samples from a riverside alluvial aquifer underneath an agricultural area in Osong, central Korea, were performed in this study to understand the spatial controls of nitrate concentrations in terms of biogeochemical processes occurring near oxbow lakes within a fluvial plain. Nitrate concentrations in groundwater showed a large variability from 0.1 to 190.6 mg/L (mean = 35.0 mg/L) with significantly lower values near oxbow lakes. The evaluation of hydrochemical data indicated that the groundwater chemistry (especially, degree of nitrate contamination) is mainly controlled by two competing processes: 1) agricultural contamination and 2) redox processes. In addition, results of factorial kriging, consisting of two steps (i.e., co-regionalization and factor analysis), reliably showed a spatial control of the concentrations of nitrate and other redox-sensitive species; in particular, significant denitrification was observed restrictedly near oxbow lakes. The results of this study indicate that sub-oxic conditions in an alluvial groundwater system are developed geologically and geochemically in and near oxbow lakes, which can effectively enhance the natural attenuation of nitrate before the groundwater discharges to nearby streams. This study also demonstrates the usefulness of multivariate statistical analysis in groundwater study as a supplementary tool for interpretation of complex hydrochemical data sets. 相似文献
7.
Omar Ali Al-Khashman 《The Environmentalist》2008,28(3):203-215
The present study investigates the physical, chemical, and biological characteristics of spring water samples in Shoubak area
in the southern Jordan. The samples were collected from May 2004 to May 2005. All samples were analyzed for temperature, conductivity,
dissolved oxygen, pH, major cations (Ca2+, Mg2+, K+, Na+), major anions (Cl−, NO3−, HCO3−, SO42−, PO43−, F−), and trace metals (Fe2+, Al3+, Mn2+, Cu2+, Cr3+, Ni2+, Zn2+, Pb2+, Cd2+). Water quality for available springs showed high salinity through long period of contact with rocks. The ion concentrations
in the water samples were from dissolution of carbonate rocks and ion exchange processes in clay. The general chemistry of
water samples was typically of alkaline earth waters with prevailing bicarbonate chloride. Some springs showed elevated nitrate
and sulfate contents which could reflect to percolation from septic tanks, cesspools, and agricultural practices. The infiltration
of wastewater from cesspools and septic tanks into groundwater is considered the major source of water pollution. The results
showed that there were great variations among the analyzed samples with respect to their physical, chemical and biological
parameters, which lie below the maximum permissible levels of the Jordanian and WHO drinking water standards. The results
indicate that the trace metals of spring’s water of Shoubak area do not generally pose any health or environmental problems.
Factor analysis was used to identify the contributers to water quality. The first factor represents major contribution from
anthropogenic activities, while the second one represents major contribution from natural processes. 相似文献
8.
F. P. Sival A. P. Grootjans P. J. Stuyfzand T. Verschoore de la Houssaye 《Journal of Coastal Conservation》1997,3(1):79-86
Basiphilous, open, species-rich vegetation types of young dune slacks have declined throughout Europe in recent years, and
have largely been replaced by often acidophilous, tall marsh and scrub vegetation. This succession appears to be accelerated
by a decrease in the discharge of calcareous groundwater from sandy ridges or small dune hummocks. The present study deals
with spatial and temporal variation in the chemical composition of the groundwater in the upper metres of the soil of a degraded
dune slack complex on the Dutch barrier island of Schiermonnikoog, with emphasis on (1) groundwater composition, (2) water
level and (3) decalcification patterns. The main aim was to assess perspectives for restoring basiphilous vegetation types
which had been abundant in this slack from 1954 to 1977. The depth of decalcification was related to former hydrological conditions
along a transect of 200 m. Acidifying effects of rainfall were reflected in the chemical composition of the groundwater below
small dune hummocks within the slack. Distinct precipitation water lenses, poor in dissolved ions, were formed under the dune
hummocks during a wet period. This microtopography did not contribute to the discharge of calcareous groundwater to lowlying
parts of the slack. Here, groundwater showed decreasing concentrations of the dissolved ions after a rain shower. Except for
the peripheral sections of the slack—where upward seepage of groundwater (exfiltration)still occurs—infiltration conditions
are now dominant in the slack. The consequences of the present hydrological conditions for restoration are briefly discussed. 相似文献
9.
Jalali M 《Environmental geochemistry and health》2007,29(5):357-374
The Faminin area in the semi-arid Hamadan state, western Iran is facing a serious deficiency in groundwater resources due
to an increasing demand associated with rapid population growth and agricultural development. The chemical composition of
78 well samples throughout the Faminin area was determined with the aim of evaluating the concentration of the background
ions and identifying the major hydrogeochemical processes that control the groundwater chemistry. The similarity between rock
and groundwater chemistries in the recharge area indicates a significant rock-water interaction. The hydrochemical types Na–HCO3 and Na–SO4 are the predominate forms in the groundwater, followed by water types Ca–HCO3 and Na–Cl. The high values of electrical conductivity and high concentrations of Na+, Cl−, SO42− and NO3− in the groundwater appeared to be caused by the dissolution of mineral phases and would appeared to be caused by anthropogenic
activities, such as intense agricultural practices (application of fertilizers, irrigation practice), urban and industrial
waste discharge, among others. 相似文献
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