Sathish Vilvanathan, Chandrasekaran Ananthanarayanan, Hamideen Mefleh Salameh, Isinkaye Mathew Omoniyi
Department of Physics, Sri Sivasubramaniya Nadar College of Engineering (Autonomous), Kalavakkam, Chennai, 603 110, India.
Department of Physics and Applied Sciences, Al-Balqa Applied University, Amman, Jordan.
Sci Rep. 2025 Jul 1;15(1):20973. doi: 10.1038/s41598-025-06142-2.
This study investigates the elemental composition, mineral distribution, and surface morphology of lake sediments from Puliyanthangal Lake, located in the Ranipet industrial area of Tamil Nadu, India. A variety of analytical techniques were employed, including Fourier-transform infrared spectroscopy (FT-IR), X-ray diffraction (XRD), energy-dispersive X-ray spectroscopy (EDS), and scanning electron microscopy (SEM). Granulometric distribution (% of sand, silt, and clay), alongside pH and electrical conductivity (EC) of sediment samples were assessed to evaluate sediment quality. FT-IR analysis identified quartz as a major mineral, evidenced by strong peaks at 779 cm, 780 cm, and 796 cm, while absorption bands between 1030 and 1035 cm, 1115 cm, and 3620-3623 cm, along with 3694 cm, confirmed the presence of clay minerals. Additionally, minor minerals such as feldspar, calcite, and organic carbon were detected through FT-IR and corroborated by XRD findings. The relative mineral distribution was further analyzed through the calculation of extinction coefficients. SEM imaging demonstrated variability in both the morphology and amorphous characteristics of the sediments, while EDS analysis highlighted the significance of certain elements implicated in the mineral formation. Furthermore, multivariate statistics revealed that the heavy metal's concentration in the sediments are attributable to anthropogenic activities, particularly the discharge of industrial wastewater.
本研究调查了位于印度泰米尔纳德邦拉尼佩特工业区的普利扬坦加尔湖湖底沉积物的元素组成、矿物分布和表面形态。采用了多种分析技术,包括傅里叶变换红外光谱(FT-IR)、X射线衍射(XRD)、能量色散X射线光谱(EDS)和扫描电子显微镜(SEM)。评估了沉积物样本的粒度分布(砂、粉砂和粘土的百分比)以及pH值和电导率(EC),以评估沉积物质量。FT-IR分析确定石英是主要矿物,在779厘米、780厘米和796厘米处有强峰证明了这一点,而在1030至1035厘米、1115厘米以及3620 - 3623厘米之间的吸收带,连同3694厘米处的吸收带,证实了粘土矿物的存在。此外,通过FT-IR检测到了长石、方解石和有机碳等次要矿物,并得到了XRD结果的证实。通过计算消光系数进一步分析了相对矿物分布。SEM成像显示了沉积物形态和非晶态特征的变异性,而EDS分析突出了某些与矿物形成有关的元素的重要性。此外,多变量统计表明,沉积物中的重金属浓度归因于人为活动,特别是工业废水的排放。