Jin-Mei Zhou1,2,3, Zhong-Cheng Jiang1,3,4, Xiao-Qun Qin1,3, Lian-Kai Zhang1,3, Qi-Bo Huang1, Guang-Li Xu2. 1. Institute of Karst Geology, Chinese Academy of Geological Sciences, Guilin 541004, China. 2. Faculty of Engineering, China University of Geosciences, Wuhan 430074, China. 3. Key Laboratory of Karst Ecosystem and Treatment of Rocky Desertification, Ministry of Natural Resources, Guilin 541004, China. 4. Key Laboratory of Karst Dynamics, Ministry of Natural Resources, Guilin 541004, China.
Abstract
Karst water is rich in calcium ions (Ca2+) and exhibits poor metal availability and low biodegradation efficiency. This study sought to analyze the effects and mechanisms of Ca2+ on lead (Pb) removal and absorption by Eichhornia crassipes (a floating plant common in karst areas). Moreover, the morphology and functional groups of E. crassipes in water were characterized via SEM, and FTIR. The results demonstrated that the removal rate of Pb in karst water (85.31%) was higher than that in non-karst water (77.04%); however, the Pb bioconcentration amount (BCA) in E. crassipes roots in karst water (1763 mg/kg) was lower than that in non-karst water (2143 mg/kg). With increased Ca2+ concentrations (60, 80, and 100 mg/L) in karst water, the Pb removal rate increased (85.31%, 88.87%, and 92.44%), the Pb BCA decreased (1763, 1317, and 1095 mg/kg), and the Ca BCA increased (6801, 6955, and 9368 mg/kg), which was attributed to PbCO3 and PbSO4 precipitation and competitive Ca and Pb absorption. High Ca2+ concentrations increased the strength of cation exchange, alleviated the fracture degree of fibrous roots, reduced the atrophy of vascular bundles, protected the cell wall, promoted C-O combined with Pb, enhanced the strength of O‒H, SO42-, C=O, and reduced the oxidization of alkynyl acetylene bonds.
Karst water is rich in pan class="Chemical">calcium ions (Ca2+) and exhibits poor metal availability and low biodegradation efficiency. This study sought to analyze the effects and mechanisms of Ca2+ on lead (Pb) removal and absorption by Eichhornia crassipes (a floating plant common in karst areas). Moreover, the morphology and functional groups of E. crassipes in water were characterized via SEM, and FTIR. The results demonstrated that the removal rate of Pb in karst water (85.31%) was higher than that in non-karst water (77.04%); however, the Pb bioconcentration amount (BCA) in E. crassipes roots in karst water (1763 mg/kg) was lower than that in non-karst water (2143 mg/kg). With increased Ca2+ concentrations (60, 80, and 100 mg/L) in karst water, the Pb removal rate increased (85.31%, 88.87%, and 92.44%), the PbBCA decreased (1763, 1317, and 1095 mg/kg), and the Ca BCA increased (6801, 6955, and 9368 mg/kg), which was attributed to PbCO3 and PbSO4 precipitation and competitive Ca and Pb absorption. High Ca2+ concentrations increased the strength of cation exchange, alleviated the fracture degree of fibrous roots, reduced the atrophy of vascular bundles, protected the cell wall, promoted C-O combined with Pb, enhanced the strength of O‒H, SO42-, C=O, and reduced the oxidization of alkynyl acetylene bonds.
Entities:
Keywords:
Eichhornia crassipes; alleviation; calcium ion (II); cation exchange; functional groups; lead
Authors: Lei Wu; Guijian Liu; Chuncai Zhou; Rongqiong Liu; Shanshan Xi; Chunnian Da; Fei Liu Journal: Environ Sci Pollut Res Int Date: 2017-10-19 Impact factor: 4.223
Authors: Jin-Mei Zhou; Zhong-Cheng Jiang; Xiao-Qun Qin; Lian-Kai Zhang; Qi-Bo Huang; Guang-Li Xu; Dionysios D Dionysiou Journal: Int J Environ Res Public Health Date: 2020-07-26 Impact factor: 3.390