Tree species effects on soil properties in experimental plantations in tropical moist forest

被引:103
作者
Russell, A. E. [1 ]
Raich, J. W.
Valverde-Barrantes, O. J.
Fisher, R. F.
机构
[1] Iowa State Univ, Dept Nat Resource Ecol & Management, Ames, IA 50011 USA
[2] Iowa State Univ, Dept Ecol Evolut & Organismal Biol, Ames, IA 50011 USA
[3] Texas A&M Univ, College Stn, TX 77843 USA
关键词
D O I
10.2136/sssaj2006.0069
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
We resampled one of the earliest replicated experimental sites used to investigate the impacts of native tropical tree species on soil properties, to examine longer term effects to 1-m depth. The mono-dominant stands, established in abandoned pasture in 1988 at La Selva Biological Station, Costa Rica, contained six species, including one exotic, Pinus patula ssp. tecunumanii (Eguiluz & J.P. Perry) Styles, and five native species: Pentaclethra macroloba (Willd.) Ktze (N-2-fixing); Hyeronima alchorneoides Allemao; Virola koschnyi Warb.; Vochysia ferruginea Mart.; and Vochysia guatemalensis J.D. Smith. Soil organic carbon (SOC) differed significantly among species in the surface (0-15-cm) layer, ranging from 44.5 to 55.1 g kg(-1), compared with 46.6 and 50.3 g kg(-1) in abandoned pasture and mature forest, respectively. The change in surface SOC over 15 yr ranged from -0.03 to 0.66 Mg C ha(-1) yr(-1). The species differed in the quantity and chemical composition of their detrital production. Soil organic C was significantly correlated with fine-root growth, but not with aboveground detrital inputs. Soil organic C increased with potential C mineralization on a grams of C basis, indicating that species influenced both the quality and quantity of SOC. Contrary to expectations, SOC declined with increasing fine-root lignin concentrations, indicating that lignin-derived C did not dominate refractory SOC pools. We hypothesize that differences among species in the capacity to increase SOC stocks involved fine-root traits that promoted soil microbial turnover and, thus, greater production of recalcitrant, microbial-derived C fractions.
引用
收藏
页码:1389 / 1397
页数:9
相关论文
共 68 条
[21]  
GONZALEZ JE, 1994, FOREST ECOL MANAG, V70, P159, DOI 10.1016/0378-1127(94)90083-3
[22]   TURNOVER OF SOIL ORGANIC-MATTER AND STORAGE OF CORN RESIDUE CARBON ESTIMATED FROM NATURAL C-13 ABUNDANCE [J].
GREGORICH, EG ;
ELLERT, BH ;
MONREAL, CM .
CANADIAN JOURNAL OF SOIL SCIENCE, 1995, 75 (02) :161-167
[23]   The potential of plantations to foster woody regeneration within a deforested landscape in lowland Costa Rica [J].
Haggar, J ;
Wightman, K ;
Fisher, R .
FOREST ECOLOGY AND MANAGEMENT, 1997, 99 (1-2) :55-64
[24]   ALUMINUM ACCUMULATION BY SOME CERRADO NATIVE SPECIES OF CENTRAL BRAZIL [J].
HARIDASAN, M .
PLANT AND SOIL, 1982, 65 (02) :265-273
[25]  
Hartshorn Gary S., 1994, P73
[26]  
Heal O. W., 1997, P3
[27]  
Hobbie SE, 2006, ECOLOGY, V87, P2288, DOI 10.1890/0012-9658(2006)87[2288:TSEODA]2.0.CO
[28]  
2
[29]   Patterns and mechanisms of soil acidification in the conversion of grasslands to forests [J].
Jobbágy, EG ;
Jackson, RB .
BIOGEOCHEMISTRY, 2003, 64 (02) :205-229
[30]   Kinetics of malate transport and decomposition in acid soils and isolated bacterial populations: The effect of microorganisms on root exudation of malate under Al stress [J].
Jones, DL ;
Prabowo, AM ;
Kochian, LV .
PLANT AND SOIL, 1996, 182 (02) :239-247