Water repellency of Casuarina windbreaks (Casuarina equisetifolia Forst.) caused by fungi in central Taiwan

被引:19
作者
Lin, CY
Chou, WC
Tsai, JS
Lin, WT
机构
[1] Chung Hua Univ, Dept Civil Engn & Engn Informat, Hsinchu 300, Taiwan
[2] Natl Chung Hsing Univ, Dept Soil & Water Conservat, Taichung 402, Taiwan
[3] Chung Hua Univ, Dept Landscape Architecture, Hsinchu 300, Taiwan
[4] Ming Dao Univ, Inst Environm Planning & Design, Peetow 523, Changhua County, Taiwan
关键词
water repellent layer; Casuarina plantation; fungi; humic substance;
D O I
10.1016/j.ecoleng.2005.10.010
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
The water repellent layer (WRL) in the Casuarina plantation near Taichung Harbor in central Taiwan is mainly due to the development of filamentous fungi. The hyphae of the isolated fungi and the metabolites of the TCHC-5 and TCHC-20 fungi are also significantly hydrophobic. In the soil layers, humic Substances decrease the phosphorus fixation and contribute to the formation of WRL. The hydrophobic properties of humic substances are unfavorable for the nutrient cycling in this area. The water contact angles of fulvic acids and humic acids are pH-dependent. Increasing the solution pH value reduces the hydrophobic strength for fulvic acids and/or humic acids. TCHC-15 and TCHC-16 isolated fungi exude strong acidic metabolites (pH 2.7-3.0). This may result in polymerization and/or precipitation of fulvic acids and humic acids and increase the hydrophobic strength of the soil layers. Humic substances with aliphatic chains are the main components that form WRL in soils. Soil pH may be an indicator of the hydrophobic potential for organic matters. (c) 2005 Elsevier B.V. All rights reserved.
引用
收藏
页码:283 / 292
页数:10
相关论文
共 40 条
[1]  
Aiken G.R., 1985, Humic Subtances in Soil, Sediment, and Water: Geochemistry, Isolation, and Characterization, P363, DOI DOI 10.1002/GJ.3350210213
[2]   Development and application of a new sessile drop contact angle method to assess soil water repellency [J].
Bachmann, J ;
Ellies, A ;
Hartge, KH .
JOURNAL OF HYDROLOGY, 2000, 231 :66-75
[3]   Physics of water repellent soils [J].
Bauters, TWJ ;
Steenhuis, TS ;
DiCarlo, DA ;
Nieber, JL ;
Dekker, LW ;
Ritsema, CJ ;
Parlange, JY ;
Haverkamp, R .
JOURNAL OF HYDROLOGY, 2000, 231 :233-243
[4]   MODELING MOVEMENT OF CHEMICALS IN SOILS BY WATER [J].
BOAST, CW .
SOIL SCIENCE, 1973, 115 (03) :224-230
[5]  
BOND R. D., 1964, AUSTRALIAN J SOIL RES, V2, P123, DOI 10.1071/SR9640123
[6]  
Bremner J.M., 1982, Methods of Soil Analysis, VSecond, P595
[7]   Water repellency in sandy luvisols under different forest transformation stages in northeast Germany [J].
Buczko, U ;
Bens, O ;
Fischer, H ;
Hüttl, RF .
GEODERMA, 2002, 109 (1-2) :1-18
[8]  
CAGAUAN BG, 1969, THESIS U HAWAII HON
[9]   UTILIZATION OF MICROBIAL SIDEROPHORES IN IRON ACQUISITION BY OAT [J].
CROWLEY, DE ;
REID, CPP ;
SZANISZLO, PJ .
PLANT PHYSIOLOGY, 1988, 87 (03) :680-685
[10]  
De Santo AV, 2002, ACTA OECOL, V23, P247, DOI 10.1016/S1146-609X(02)01155-4