铁铝土对溶解性有机质的吸附特性
Adsorption of dissolved organic matter on ferrallitic soils
-
摘要: 采用批实验方法,结合XAD树脂分组技术研究铁铝土对3种不同亲/疏性DOM(堆肥DOM、秸秆DOM、土壤DOM)的吸附特征并分析其影响因素.结果表明:(1)铁铝土对DOM具有强吸附力,吸附量随DOM初始浓度的增加而增加,吸附动力学包括快吸附和慢吸附两个阶段,符合一级扩散方程;(2)等温吸附特征符合Freundlich方程,为物理作用主导的多层吸附过程;(3)对于同种DOM,铁铝土对DOM的吸附量表现为暗红湿润铁铝土> 简育铁铝土> 潜育水稻土,对50 mg·L-1的堆肥DOM在暗红湿润铁铝土的吸附量达594.9 mg·kg-1,与CEC、游离氧化铁、游离氧化铝、粘粒呈极显著正相关,与砂粒呈负相关;(4)对于同种铁铝土,高疏水性DOM在铁铝土吸附量更大,表现为堆肥DOM(H-DOM)> 土壤DOM(M-DOM)> 秸秆DOM(L-DOM);(5)铁铝土对DOM各组分的吸附力表现为疏水中性组分(HON)> 酸不溶组分(AIM)> 疏水碱性组分(HOB)> 疏水酸性组分(HOA)> 亲水性组分(HIM),结合各组分的红外光谱特征,推测脂肪链状结构、高芳香性是影响吸附量的关键.(6)DOM各组分对DOM吸附量的贡献是各组分吸附能力与含量的综合作用结果.对于亲疏水性组分,HO对DOM吸附量的贡献大于HIM,达69.43%—85.08%;对于各极性-电荷特性组分,表现为H-DOM:HOA(40.24%)> HON(39.1%)> HIM(14.92%)> AIM(3.82%)> HOB(1.88%);L-DOM:HOA(33.50%)> HIM(30.57%)> HON(24.81%)> AIM(7.45%)> HOB(3.68%).(7)内源DOM对铁铝土吸附外源DOM起抑制作用,且对高疏水性的DOM抑制作用更强.Abstract: Batch experiments and XAD resin were used to investigate dissolved organic matter (DOM) adsorption by ferrallitic soils. The effects of soil properties and DOM characteristics on the adsorption were also studied to reveal the adsorption mechanism. The results showed that: (1) ferrallitic soils had high DOM adsorption capacity, which increased with initial DOM concentrations. The kinetics of DOM adsorption in the ferrallitic soils can be divided into the two stages: fast and slow reactions, and it could be better fitted by frist-order model; (2) the adsorption isotherms of DOM on ferrallitic soils could be better fitted by Freundlich equation, indicating the adsorption process was a physical multilayer adsorption process; (3) for different soils, the adsorption capacity of DOM follows the order of rhodic ferralsol > haplic ferralsol > paddy soil, adsorbing capacity of compost DOM was up to 594.9 mg·kg-1 in the initial concentration of 50 mg·L-1, it positively correlated with CEC, free iron oxide, free aluminium oxide and clay content, while negatively correlated with sand content; (4) for different DOMs, more hydrophobic DOM had the larger adsorption capacity, which follows the order of compost DOM (H-DOM) > soil DOM (M-DOM) > straw DOM(L-DOM); (5) for different DOM components, the adsorption capacity decreased as follows: hydrophobic neutrals (HON) > acid-insoluble matter (AIM) > hydrophobic bases (HOB) > hydrophobic acids (HOA) > hydrophillic matter (HIM). And the chain structure of aliphatic alkanes and higher aromaticity in DOM were the key factors influencing adsorption capacity as revealed by Fourier-transform infrared spectroscopy (FT-IR); (6) the contribution to DOM adsorption by different fractions was the result of their adsorption capacity and content. For different hydrophobic DOM, hydrophobic matter's contribution (HO) was more than HIM, up to 69.43%—85.08%. For different polar fractions, H-DOM: HOA(40.24%)> HON(39.1%)> HIM(14.92%)> AIM(3.82%)> HOB(1.88%); L-DOM: HOA(33.50%)> HIM(30.57%)> HON(24.81%)> AIM(7.45%)> HOB(3.68%). (7) the presence of exogenous DOMs in soil impeded the exogenous DOM adsorption by soil, especially for more hydrophobic DOM.
-
Key words:
- dissolved organic matter /
- ferrallitic soils /
- adsorption /
- affecting factor
-
[1] KALBITZ K, SOLINGER S, PARK J H, MICHALZIK B, et al. Controls on the dynamics of dissolved organic matter in soils [J].Soil Science, 2000, 165(4): 277-304. [2] 赵劲松, 张旭东, 袁星, 等. 土壤溶解性有机质的特性与环境意义[J]. 应用生态学报, 2003, 14(1):126-130. ZHAO J S, ZHANG X D, YUAN X, et al. Characteristics and environmental significance of soil dissolved organic matter [J]. Chinese Journal of Applied Ecology, 2003, 14(1):126-130 (in Chinese).
[3] 康露, 吴景贵, 赵欣宇. 吉林省两种土壤对水溶性有机物吸附-解吸的影响因素[J]. 东北林业大学学报, 2013,41(8): 130-135. KANG L, WU J G, ZHAO X Y. Adsorption and desorption of dissolved organic matter and its influencing factors on two types of soil in Jilin Province, China [J]. Journal of Northeast Forestry University. 2013, 41(8):130-135 (in Chinese).
[4] ANNELENE P, LINE K J, JAN M, et al. Potential adsorption of dissolved organic matter in poorly podzolised, high-latitude soils [J]. Geoderma, 2014, 226–227: 39–46. [5] OREN A, CHEFETZ B. Sorptive and desorptive fractionation of dissolved organic matter by mineral soil matrices [J]. Journal of Environmental Quality, 2012, 41:526-533. [6] 龚子同, 张甘霖, 漆智平. 海南省土系概论[M]. 北京: 科学出版社, 2004. GONG Z T, ZHANG G L, QI Z P. Introduction to soil series of Hainan Province, China [M]. Beijing: Science Press, 2004 (in Chinese). [7] KAISER K, GUGGENBERGER G. The role of DOM sorption to mineral surfaces in the preservation of organic matter in soils [J]. Organic Geochemistry, 2000, 31:711-725. [8] KOTHAWALA D N, ROEHM C, BLODAU, et al. Selective adsorption of dissolved organic matter to mineral soils [J]. Geoderma, 2012, 189-190: 334-342. [9] 吴济舟. 溶解性有机质分组及各组分对芘的生物有效性及其吸附解吸的影响研究[D]. 天津: 南开大学, 2012. WU J Z. Fractionation of dissolved organic matter and the impact of the fractions on the bioavailability and sorption-desorption of pyrene [D]. Tianjin: Nankai University, 2012 (in Chinese). [10] 倪文海, 刘欢, 刘振涛,等. 水稻秸杆腐解过程溶解性有机质红外光谱研究[J]. 土壤, 2013, 45 (2): 220-226. NI W H, LIU H, LIU Z T, et al, Study on fourier-transform infrared spectra of dissolved organic matters extracted from rice straw at different decay stages[J]. Soils, 2013, 45 (2): 220-226 (in Chinese).
[11] 凌婉婷. 溶解性有机质对莠去津在土壤/矿物-水界面行为的影响及其机理研究[D]. 杭州: 浙江大学, 2005. LING W T. The influence of dissolved organic matter on atrazine sorption and desorption by soils and minerals [D]. Hangzhou: Zhejiang University, 2005 (in Chinese). [12] 汤智, 赵晓丽, 吴丰昌, 等. 不同来源腐殖酸在纳米四氧化三铁上的吸附及对其沉降性的影响[J]. 环境化学, 2015, 34(8):1520-1528. TANG Z, ZHAO X L, WU F C, et al. The interaction between Fe3O4 nanoparticle and different source humic acid, and the influence on nanoparticle suspension [J]. Environmental Chemistry, 2015, 34(8): 1520-1528 (in Chinese).
[13] 周江敏, 代静玉, 潘根兴, 等. 应用光谱分析技术研究土壤水溶性有机质的分组及其结构特征[J]. 光谱学与光谱分析, 2004, 24(9):1060-1065. ZHOU J M, DAI J Y, PAN G X, et al. Fractionation and spectroscopic property of dissolved organic matters in soils [J].Spectroscopy and Spectral Analysis, Spectroscopy and Spectral Analysis, 2004, 24(9):1060-1065 (in Chinese).
[14] 韩成卫, 李忠佩, 刘丽, 等. 溶解性有机碳在红壤水稻土中的吸附及其影响因素[J]. 生态学报, 2008, 28 (1): 445-451. HAN C W, LI Z P, LIU L, et al. Adsorption of dissolved organic carbon on paddy soils of subtropical China [J]. Acta Ecologica sinica, 2008, 28 (1): 445-451(in Chinese).
[15] 许中坚, 刘广深, 刘维屏. 土壤中溶解性有机质的环境特性与行为[J]. 环境化学, 2003,22(5):427-433. XU Z J, LIU, G S, LIU W P. Environmental characteristic and behavior of dissolved organic matter in soils[J]. Environmental Chemistry, 2003,22(5):427-433 (in Chinese).
[16] 方艳芬, 李新玉, 周薇, 等. 黄铁矿对水体中腐殖酸的吸附特性[J]. 环境化学, 2014, 33(11): 1941-1949. FANG Y F, LI X Y, ZHOU W, et al. Adsorption characteristics of humic acids on pyrite in water [J]. Environmental Chemistry, 2014, 33(11):1941-1949 (in Chinese).
[17] 程和发, 胡二丹, 韦昌富. 矿物微孔对有机污染物吸附的机理和影响因素[J]. 矿物岩石地球化学通报, 2015, 34(2): 250-256. CHENG H F, HU E D, WEI C F. Sorption of organic contaminants in mineral micropores: Mechanism and major controlling factors [J]. Bulletin of mineralogy petrology and geochemistry, 2015, 34(2): 250-256 (in Chinese).
计量
- 文章访问数: 988
- HTML全文浏览数: 906
- PDF下载数: 501
- 施引文献: 0