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植酸对碳酸盐绿锈转化的影响

Effects of myo-inositol hexakisphosphate on the transformation of carbonate green rust
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摘要 为研究植酸(IHP)对绿锈转化过程及机制的影响,通过空气氧化法合成碳酸盐绿锈[GR1(CO_(3)^(2-))],并利用X射线衍射、衰减全反射-傅里叶变换红外光谱、高分辨透射电子显微镜、扫描电子显微镜和能量色散X射线能谱对体系中的固体产物进行分析表征。研究表明:不存在IHP时GR1(CO_(3)^(2-))在5 h左右完全转化为针铁矿,而存在IHP时GR1(CO_(3)^(2-))的转化会受到抑制。在0~0.5 mmol·L^(-1)的IHP浓度范围内,GR1(CO_(3)^(2-))的转化产物为针铁矿,而当IHP浓度高于1.0 mmol·L^(-1)时,GR1(CO_(3)^(2-))的转化产物为针铁矿和高铁绿锈。IHP对GR1(CO_(3)^(2-))转化机制的影响与其浓度有直接关系,在低浓度IHP(0~0.5 mmol·L^(-1))条件下,GR1(CO_(3)^(2-))转化过程只涉及溶解-氧化-沉淀(DOP)机制;而高浓度IHP(1.0~5.0 mmol·L^(-1))体系中,固态氧化(SSO)机制占主导地位,在其转化过程中,一部分GR1(CO_(3)^(2-))通过溶解再沉淀机制转化为针铁矿,一部分GR1(CO_(3)^(2-))通过原位脱质子反应转化为高铁绿锈。此外,在GR1(CO_(3)^(2-))转化过程中,IHP在GR1(CO_(3)^(2-))及其转化产物表面会形成内圈络合物和植酸(亚)铁沉淀。总体而言,IHP会抑制GR1(CO_(3)^(2-))的溶解再沉淀转化机制,阻碍针铁矿的结晶和晶体生长,且抑制作用与IHP浓度呈正相关。 Green rust exists widely in paddy soil,sediment,groundwater,and other environments,and its transformation is affected by various environmental geochemical factors.Carbonate green rust[GR1(CO_(3)^(2-))]was synthesized by air oxidation,and the effect of organic phosphorus(myo-inositol hexakisphosphate,IHP)on the transformation process and mechanism of green rust was investigated.The solid products in the system were characterized by X-ray diffraction,attenuated total reflection Fourier-transform infrared spectroscopy,highresolution transmission electron microscopy,scanning electron microscopy,and energy dispersive X-ray spectroscopy.The results showed that GR1(CO_(3)^(2-))was completely converted to goethite in approximately 5 h in the absence of IHP,while the transformation of GR1(CO_(3)^(2-))was inhibited in the presence of IHP.In the presence of 0-0.5 mmol·L^(-1) IHP,the transformation product of GR1(CO_(3)^(2-))was goethite,while GR1(CO_(3)^(2-))was transformed into goethite and ferric green rust when the concentration of IHP was above 1.0 mmol·L^(-1).The effect of IHP on the conversion mechanism of GR1(CO_(3)^(2-))was directly related to its concentration.In a system with a low concentration of IHP(0-0.5 mmol·L^(-1)),the conversion process of GR1(CO_(3)^(2-))only involved the dissolution-oxidation-precipitation(DOP)mechanism.However,in a system with a high concentration of IHP(1.0-5.0 mmol·L^(-1)),the solid-state oxidation(SSO)mechanism dominated,and GR1(CO32-)was partially converted into goethite through a dissolution reprecipitation mechanism,and GR1(CO_(3)^(2-))was partially transformed into ferric green rust via an in situ deprotonation reaction.In addition,during the transformation of GR1(CO_(3)^(2-)),IHP formed inner-sphere complexes or(ferro)ferric phytate precipitates on the surface of GR1(CO_(3)^(2-))and its transformation products.Overall,IHP inhibites the dissolutionreprecipitation transformation mechanism of GR1(CO_(3)^(2-))and hinderes the crystallization and crystal growth of goethite,and the inhibition is positively correlated with the concentration of IHP.
作者 孙亚丽 姜冠杰 江睿 兰帅 李阳 严玉鹏 张嵚 SUN Yali;JIANG Guanjie;JIANG Rui;LAN Shuai;LI Yang;YAN Yupeng;ZHANG Qin(College of Land Resources and Environment,Jiangxi Agricultural University,Nanchang 330045,China;Key Laboratory of Poyang Lake Watershed Agricultural Resources and Ecology of Jiangxi Province,Nanchang 330045,China)
出处 《农业环境科学学报》 CAS CSCD 北大核心 2023年第2期393-402,共10页 Journal of Agro-Environment Science
基金 国家自然科学基金项目(42167031)。
关键词 碳酸盐绿锈 植酸 转化 针铁矿 高铁绿锈 carbonate green rust myo-inositol hexakisphosphate transformation goethite ferric green rust
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  • 1Antony H, Legrand L, Chausse A. Carbonate and sulphate green rusts-Mechanisms of oxidation and reduction. Electrochimica Ac- ta, 2008, 53(24) : 7146--7156.
  • 2Trolard F, Fougerite: From field experiment to the homologation of the mineral. Comptes Rendus Geoscienee, 2006, 338 (16) : 1158--1166.
  • 3Refait Ph, G6nin A, Abdelmoula M, et al. Copreeipitation ther- modynamics of iron (11-111) hydroxysulfate green rust from Fe (11) and Fe(lll) salts. Corrosion Science, 2003, 45 (4) : 659--676.
  • 4G~nin j M R, Bourrie G, Trolard F,et al. Thermodynamic equi- libria in aqueous suspensions of synthetic and natural Fe (I1)-Fe (111) green rusts: Occurrences of the mineral in hydromorphic soils. En,~ironmeutal Science & Technology, 1998, 32 ( 8 ) :1058--1068.
  • 5Bernal J D, Dasgupta D R, Mackay A L. The oxides and hydrox- ides of iron and their structural inter-relationships. Clay Mineral Bulletin, 1959, 4:15--30.
  • 6Refait Ph, Simon L, G~nin J M R. Reduction of SeO~- anions and anoxic formation of iron ( II )-iron ( 11I ) hydroxy-selenate green rust. Environmental Science & Technology, 2000, 34(5 ) : 819--825.
  • 7Trolard F, Bourri6 G. Structure of fougerite and green rusts and a thermodynamic model for their stabilities. Journal of Geochemical Exploration, 2006, 88(1): 249--251.
  • 8Christiansen B C, Balic-Zunie T, Dideriksen K, et al. Identifi- cation of green rust in groundwater. Environmental Science & Technology, 2009, 43(10) : 3436--3441.
  • 9Hansen H C B, Koch C B, Nancke-Krogh O K, et al. Abioticni- irate reduction to ammonium: Key role of green rust. Environ- mental Science & Technology, 1996, 30(6) : 2053--2056.
  • 10Refait Ph, Abdelmoula M, G6nin J M R. Mechanisms of forma- tion and structure of green rust one in aqueous corrosion of iron in the presence of chloride ions. Corrosion Science, 1998, 40(9) : 1547--1560.

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