@Article{SantosTngApgAssMan:2022:SoPhFr,
author = "Santos, Emily Darc Andrade dos and Tng, David Yue Phin and Apgaua,
Deborah Mattos Guimar{\~a}es and Assun{\c{c}}{\~a}o, Raul Reis
and Manzi, Antonio Ocimar",
affiliation = "{Instituto Nacional de Pesquisas da Amaz{\^o}nia (INPA)} and
{Centre for Rainforest Studies} and {Centre for Rainforest
Studies} and {Universidade Federal de Lavras (UFLA)} and
{Instituto Nacional de Pesquisas Espaciais (INPE)}",
title = "Soil phosphorus fractions and their relation to leaf litterfall in
a central Amazonian terra firme rainforest",
journal = "Acta Amazonica",
year = "2022",
volume = "52",
number = "2",
pages = "104--113",
keywords = "leaf litter, nutrient cycling, tropical soil.",
abstract = "Phosphorus (P) cycling is an important yet poorly studied aspect
of the macronutrient balance in tropical rainforest ecosystems. As
soil P occurs in different organic and inorganic forms (fractions)
with varying degrees of lability, we hypothesized that these
fractions will vary between soil types, and temporally within soil
types. Additionally, we hypothesized a direct influence of leaf
litterfall P input on soil total P and soil P fractions. We
collected soil and leaf litter samples from three soil types in a
central Amazonian lowland rainforest in Brazil over five months,
and used a modified Hedleys fractionation method to determine six
organic and inorganic soil P fractions, and also total, labile and
residual P. Leaf litterfall P concentrations were determined
colorimetrically. Soil inorganic and organic P fractions varied
between soil types and across months, but soil type and month
interactions were mostly non-significant. Some inorganic P
fractions (Pi-NaOH) peaked while the organic fractions (Po-NaOH)
fell and vice versa. Leaf litterfall production and leaf
litterfall P input peaked around two months following the wettest
month. Leaf litterfall P input was a significant predictor of
Po-NaHCO3, a bioavailable P fraction. Future studies on P cycling
in terrestrial ecosystems should examine the roles played by
individual soil P fractions as they cycle asynchronistically and
differently across soil types.",
doi = "10.1590/1809-4392202103471",
url = "http://dx.doi.org/10.1590/1809-4392202103471",
issn = "0044-5967",
language = "en",
targetfile = "download.pdf",
urlaccessdate = "23 maio 2024"
}