土壤学
热带亚热带干阔叶林
热带
农林复合经营
旱季
生态学
热带森林
生物
地理
林业
环境科学
土壤水分
作者
Jennifer S. Powers,Daniel Peréz‐Aviles
出处
期刊:Biotropica
[Wiley]
日期:2012-05-14
卷期号:45 (1): 1-9
被引量:48
标识
DOI:10.1111/j.1744-7429.2012.00881.x
摘要
Abstract Although there are generalized conceptual models that predict how above and belowground biomass increase during secondary succession after abandonment from agriculture, there are few data to test these models for fine roots (defined as ≤2 mm diameter) in tropical forests. We measured live and dead fine roots (0–10 cm depth) in 18 plots of regenerating tropical dry forest in C osta R ica that varied in age from 5 to 60 yrs, as well as in soil properties. We predicted that both stand age and soil fertility would affect fine roots, with greater values in older forests on low fertility soils. Across two sampling dates and locations, live fine roots varied from 0.35 to 3.53 Mg/ha and dead roots varied from 0.15 to 0.93 Mg/ha. Surprisingly, there was little evidence that surface fine roots varied between sampling dates or in relation to stand age. By contrast, total, live, and dead fine roots averaged across sampling dates within plots were negatively correlated with a multivariate index of soil fertility ( P earson correlations coefficients were −0.64, −0.58, and −0.68, respectively; P < 0.01) and other individual edaphic variables including pH , silt, calcium, magnesium, nitrogen, and phosphorus. These results suggest that soil fertility is a more important determinant of fine roots than forest age in tropical dry forests in C osta R ica, and that one‐way these plant communities respond to low soil fertility is by increasing fine roots. Thus, simple conceptual models of forest responses to abandonment from agriculture may not be appropriate for surface fine roots.
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