Sorption of DOM and DOM fractions to forest soils

被引:288
作者
Kaiser, K
Guggenberger, G
Zech, W
机构
[1] Inst. of Soil Sci. and Soil Geogr., University of Bayreuth
关键词
sorption; dissolved organic matter; dissolved organic matter fractions; soil properties;
D O I
10.1016/S0016-7061(96)00071-7
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
The sorption of total, hydrophilic, and hydrophobic dissolved organic matter (DOM)) on 125 forest soil samples was studied in batch experiments. The soil samples represented the main soil orders of temperate climatic zones: Entisols, Inceptisols, Alfisols, Mollisols, and Spodosols. In general, sorption was adequately described by the linear initial mass isotherm. At zero addition of DOM, the release of dissolved organic carbon (DOG) into solutions depended on the soil organic C (OC) content. The DOC released was comprised primarily of hydrophilic substances (61-100%). High contents of OC reduced DOC sorption, notably that of hydrophilic DOG. In soils free of carbonates, sorption was related to oxalate-extractable aluminum (Al-o) and dithionite-extractable iron (Fe-d); however, in carbonatic soils DOC retention was correlated with Fe-d only. Consequently, soils with high OC content and/or low contents of extractable Al and Fe showed low DOC retention (e.g. E horizons), whereas subsoil horizons had high DOC sorption capacities. The majority of the soils preferentially sorbed hydrophobic DOG. This was caused by the higher affinity of hydrophobic DOC to oxide/hydroxide soil components. There was also a strong competition effect between hydrophilic and hydrophobic DOC, especially in soils with a limited number of binding sites. Sorption of hydrophobic DOC in some soils was even accompanied by the displacement of indigenous hydrophilic substances. In carbonate-free soils, multiple regression analysis including Al-o, Fe-d, and OC explained 75 and 77% of the variance of the partition coefficient (m) of the initial mass isotherm for the sorption of total and hydrophobic DOC, respectively. Due to the competitive effect of hydrophobic DOC on hydrophilic DOC retention, the relation was weaker for the hydrophilic fraction. In the carbonate-containing soils, multiple regression analysis including Fe-d and OC explained 67, 58, and 59% of the variance of in for total, hydrophilic, and hydrophobic DOC, respectively.
引用
收藏
页码:281 / 303
页数:23
相关论文
共 69 条
[31]  
HUANG PM, 1986, SOIL SCI SOC AM J, V17, P159
[32]   MECHANISMS OF DISSOLVED ORGANIC-CARBON ADSORPTION ON SOIL [J].
JARDINE, PM ;
WEBER, NL ;
MCCARTHY, JF .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1989, 53 (05) :1378-1385
[33]   INTERACTIONS OF HUMIC ACIDS AND ALUMINUM SALTS IN THE FLOCCULATION PROCESS [J].
JEKEL, MR .
WATER RESEARCH, 1986, 20 (12) :1535-1542
[34]   FLOCCULATION OF KAOLINITIC SOIL CLAYS - EFFECTS OF HUMIC SUBSTANCES AND IRON-OXIDES [J].
KRETZSCHMAR, R ;
ROBARGE, WP ;
WEED, SB .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1993, 57 (05) :1277-1283
[35]   EFFECTS OF XAD-8 FRACTIONS OF DISSOLVED ORGANIC-CARBON ON THE SORPTION AND BIOAVAILABILITY OF ORGANIC MICROPOLLUTANTS [J].
KUKKONEN, J ;
MCCARTHY, JF ;
OIKARI, A .
ARCHIVES OF ENVIRONMENTAL CONTAMINATION AND TOXICOLOGY, 1990, 19 (04) :551-557
[36]  
LAHANN RW, 1980, GEOCHIM COSMOCHIM AC, V44, P337
[38]  
LYKLEMA J, 1985, FLOCCULATION SEDIMEN
[39]   CATION TYPE AND IONIC-STRENGTH EFFECTS ON THE SOLUTION COMPOSITION OF AN ACIDIC SUBSOIL [J].
MANSON, AD ;
FEY, MV .
JOURNAL OF SOIL SCIENCE, 1989, 40 (03) :577-583
[40]   SUBSURFACE TRANSPORT OF CONTAMINANTS - MOBILE COLLOIDS IN THE SUBSURFACE ENVIRONMENT MAY ALTER THE TRANSPORT OF CONTAMINANTS [J].
MCCARTHY, JF ;
ZACHARA, JM .
ENVIRONMENTAL SCIENCE & TECHNOLOGY, 1989, 23 (05) :496-502