Quantification of proton budgets in soils of cropland and adjacent forest in Thailand and Indonesia

被引:42
作者
Fujii, Kazumichi [1 ]
Funakawa, Shinya [1 ]
Hayakawa, Chie [1 ]
Sukartiningsih [2 ]
Kosaki, Takashi [3 ]
机构
[1] Kyoto Univ, Grad Sch Agr, Kyoto 6068502, Japan
[2] Mulawarman Univ, Dept Forestry, Samarinda 75123, Indonesia
[3] Kyoto Univ, Grad Sch Global Environm Studies, Kyoto 6068501, Japan
关键词
Continuous cultivation; Dissolved organic carbon; Organic matter decomposition; Proton budget; Soil acidification; Soil organic matter; NORTHERN THAILAND; HYDRAULIC CONDUCTIVITY; SHIFTING CULTIVATION; ORGANIC-MATTER; RAIN-FOREST; ACIDIFICATION; CARBON; DYNAMICS; NITROGEN; RESPIRATION;
D O I
10.1007/s11104-008-9776-0
中图分类号
S3 [农学(农艺学)];
学科分类号
0901 ;
摘要
Continuous cultivation has the potential to accelerate soil acidification. The influence of cultivation on soil acidification was evaluated by calculating proton budget in a soil-vegetation system including solute leaching, vegetation uptake and organic matter decomposition in cropland and adjacent forest in Thailand and Indonesia. In the forests, excess cation accumulation in wood (2.1-3.8 kmol(c) ha(-1) year(-1)) has contributed to soil acidification at the rate of 0.004 mol(c) for production of 1 mol carbon. In the croplands, soil organic matter loss (2.2-3.9 Mg C ha(-1) year(-1)) has contributed to both proton generation owing to nitrification (1.5-5.0 kmol(c) ha(-1) year(-1)) and proton consumption owing to mineralization of organic anions (3.6-8.8 kmol(c) ha(-1) year(-1)) at the rates of 0.008-0.015 and 0.019-0.026 mol(c) for the loss of 1 mol soil organic carbon, respectively. Although the influence of cultivation on proton budget is different depending on the budget of organic matter and soil types (soil pH and texture), cultivation results in soil organic matter loss and soil alkalinization at least during the initial stage of cultivation in tropical regions.
引用
收藏
页码:241 / 255
页数:15
相关论文
共 36 条
[1]  
[Anonymous], 2006, KEYS SOIL TAXONOMY, V10th
[2]  
[Anonymous], EXPT NAM PHROM NE TH
[3]  
Binkley D., 1987, ADV ECOL RES, V16, P1, DOI DOI 10.1016/S0065-2504(08)60086-0
[4]   PROCESSES OF SOIL ACIDIFICATION DURING NITROGEN CYCLING WITH EMPHASIS ON LEGUME BASED PASTURES [J].
BOLAN, NS ;
HEDLEY, MJ ;
WHITE, RE .
PLANT AND SOIL, 1991, 134 (01) :53-63
[5]   A global relationship between the heterotrophic and autotrophic components of soil respiration? [J].
Bond-Lamberty, B ;
Wang, CK ;
Gower, ST .
GLOBAL CHANGE BIOLOGY, 2004, 10 (10) :1756-1766
[6]   SOIL ACIDIFICATION FROM LONG-TERM USE OF ANHYDROUS AMMONIA AND UREA [J].
BOUMAN, OT ;
CURTIN, D ;
CAMPBELL, CA ;
BIEDERBECK, VO ;
UKRAINETZ, H .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1995, 59 (05) :1488-1494
[7]   INTERNAL AND EXTERNAL PROTON LOAD TO FOREST SOILS IN NORTHERN GERMANY [J].
BREDEMEIER, M ;
MATZNER, E ;
ULRICH, B .
JOURNAL OF ENVIRONMENTAL QUALITY, 1990, 19 (03) :469-477
[8]   DETERMINATION OF TOTAL SULFUR AND CHLORINE IN PLANT MATERIALS BY ION CHROMATOGRAPHY [J].
BUSMAN, LM ;
DICK, RP ;
TABATABAI, MA .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1983, 47 (06) :1167-1170
[9]   Contribution of different proton sources to pedogenetic soil acidification in forested ecosystems in Japan [J].
Fujii, Kazumichi ;
Funakawa, Shinya ;
Hayakawa, Chie ;
Kosaki, Takashi .
GEODERMA, 2008, 144 (3-4) :478-490
[10]   Ecological study on the dynamics of soil organic matter and its related properties in shifting cultivation systems of Northern Thailand [J].
Funakawa, S ;
Tanaka, S ;
Shinjyo, H ;
Kaewkhongkha, T ;
Hattori, T ;
Yonebayashi, K .
SOIL SCIENCE AND PLANT NUTRITION, 1997, 43 (03) :681-693