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首页> 外文期刊>Journal of the Indian Society of Soil Science >Application of Geoinformatics for Groundwater Characterization
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Application of Geoinformatics for Groundwater Characterization

机译:地理信息学在地下水表征中的应用

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Groundwater is the main source of irrigation in most arid and semi-arid regions of India. Therefore, there is a need to appraise quality of groundwater for sustainable crop production in these regions. In present study eighty one groundwater samples collected from tubewells across the block Gohana were analyzed for pH, electrical conductivity (EC), major cations namely, sodium (Na+), potassium (K+), calcium (Ca2+) and magnesium (Mg2+), and anions namely, carbonate (CO_3~(2-)), bicarbonate (HCOy), chloride (CI), sulphate (S042), nitrate (N03) and fluoride (F) and specific irrigation water quality indices viz., sodium adsorption ratio (SAR) and residual sodium carbonate (RSC). The pH of groundwater varied from 7.19 to 9.72 with a mean value of 8.18 and EC from 0.29 to 15.76 dS m~(-1) with a mean value of 2.74 dS m1. Among different cations, Na+ was found as the most dominant cation followed by Mg2+, Ca2+ and K+. In case of anions, CI~-was the dominant anion followed by SO_4~(2-), HCO_3~-, CO_3~(2-),N03~ and P. The SAR of groundwater varied from 4.03 to 24.16 (mmol L~(-1))~-(-2) with a mean value of 10.59 (mmol L~(-1))~-(-2) . Correlation matrix indicated that EC is highly correlated with CI~-, CO_3~(2-), SO_4~(2-), Na~+, Mg~(2+), Ca~(2+) and K+. The results from the laboratory were imported to ArcGIS (Arc Map 9.2 software) to generate the spatial variability maps of EC, SAR, RSC and water quality. The water quality map will furnish firsthand information to authorities and devisers about the groundwater quality of the study area. Hence, geoinformatics plays a pivotal role in the study of earth resources.
机译:地下水是印度大多数干旱和半干旱地区的主要灌溉来源。因此,需要在这些地区评估地下水的质量。在本研究中,将八十台从块胚芽中收集的地下水样品被分析为pH,导电性(EC),主要阳离子,钠(Na +),钾(K +),钙(Ca2 +)和镁(Mg2 +),以及阴离子即,碳酸盐(CO_3〜(2-)),碳酸氢盐(HCOY),氯化物(CI),硫酸盐(SO 42),硝酸盐(NO 3)和氟化物(F)和特定的灌溉水质索引和钠,吸附率( SAR)和残留碳酸钠(RSC)。地下水的pH从7.19至9.72变化,平均值为8.18和Ec,0.29至15.76ds m〜(-1),平均值为2.74ds m1。在不同的阳离子中,发现Na +作为最阳极的阳离子,然后是Mg2 +,Ca2 +和K +。在阴离子的情况下,CI〜-Was是优势的阴离子,然后是SO_4〜(2-),HCO_3〜 - ,CO_3〜(2 - ),N03〜和P.地下水的SAR从4.03变化到24.16(mmol l〜 (-1))〜 - ( - 2)平均值为10.59(mmol l〜(-1))〜 - ( - 2)。相关矩阵表明EC与CI〜 - ,CO_3〜(2-),SO_4〜(2-),NA +,MG〜(2+),CA〜(2+)和K +高度相关。实验室的结果被导入ArcGIS(arc Map 9.2软件),以产生EC,SAR,RSC和水质的空间变化图。水质地图将为有关研究区域的地下水质量的当局和副理者提供第一手信息。因此,地理信息学在地球资源的研究中起着枢转作用。

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