Department of Geological Engineering, Karadeniz Technical University, 61080, Trabzon, Turkey.
Environ Monit Assess. 2022 Jan 28;194(2):135. doi: 10.1007/s10661-022-09791-2.
Çarşamba aquifer is one of the most important coastal aquifers in Turkey. This aquifer is confronted by overexploitation due to the agricultural and industrial activities. The aim of the present study is to investigate the seasonal variations of hydrogeochemical parameters and to assess the suitability for drinking and irrigation of groundwater in the coastal aquifer of Çarşamba plain. For this purpose, in July and December of the year 2019, 33 and 30 groundwater samples respectively were taken from boreholes in the study area and for these samples, EC, pH, TDS, Na, Ca, K, Mg, CO, HCO, Cl, SO, NH, NO, and NO values were determined. Strong correlation was observed between Cl and Na during both seasons indicating the seawater intrusion on groundwater in the study area. Principal component analysis showed that in the study area, seawater intrusion, rock-water interaction, and anthropogenic activities from agricultural areas are the main factors that impact the groundwater chemistry. Seawater intrusion is the most important factor which affects the groundwater chemistry in July while in December, the main factor is rock-water interaction. In December, NO and NH values of most water samples exceed the authorized limits of Turkish Standard and WHO. Water quality index indicated that most of the water samples are suitable for drinking. Wilcox diagram and US salinity diagram used to evaluate the suitability of groundwater for irrigation suggested that in July, 87.87% (90% in December) (for Wilcox diagram) and 96.96% (100% in December) (for US salinity diagram) of the water samples belonged to the good to permissible class, and therefore are suitable for irrigation purpose. In addition, the EC, %Na, TH, RSC, SAR, PI, KI, and MH values of samples showed that during both seasons, most of the water samples are suitable for irrigation. However, in July, 51.52% (43.43% in December) of samples have extremely high potential salinity values, thus revealing the unsuitability of most groundwater samples for irrigation in the study area.
恰尔尚巴含水层是土耳其最重要的沿海含水层之一。由于农业和工业活动,该含水层面临过度开采的问题。本研究的目的是调查水文地球化学参数的季节性变化,并评估恰尔尚巴平原沿海含水层地下水的饮用水和灌溉适宜性。为此,在 2019 年 7 月和 12 月,分别从研究区的钻孔中采集了 33 个和 30 个地下水样本,并对这些样本测定了 EC、pH、TDS、Na、Ca、K、Mg、CO、HCO、Cl、SO、NH、NO 和 NO 值。两个季节的 Cl 和 Na 之间存在很强的相关性,表明研究区地下水受到海水入侵的影响。主成分分析表明,在研究区,海水入侵、岩石-水相互作用和农业区的人为活动是影响地下水化学的主要因素。海水入侵是 7 月影响地下水化学的最重要因素,而 12 月的主要因素是岩石-水相互作用。在 12 月,大多数水样的 NO 和 NH 值超过了土耳其标准和世界卫生组织的授权限值。水质指数表明,大多数水样适合饮用。Wilcox 图和美国盐度图用于评估地下水灌溉的适宜性,结果表明,在 7 月,87.87%(12 月为 90%)(Wilcox 图)和 96.96%(12 月为 100%)(美国盐度图)的水样属于良好到可接受的类别,因此适合灌溉用途。此外,EC、%Na、TH、RSC、SAR、PI、KI 和 MH 值的样本表明,在两个季节中,大多数水样都适合灌溉。然而,在 7 月,51.52%(12 月为 43.43%)的样本具有极高的潜在盐度值,表明研究区大多数地下水样本不适合灌溉。