1999
DOI: 10.1016/s0038-0717(98)00151-5
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Litter decomposition by four functional tree types for use in silvopastoral systems

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Cited by 77 publications
(45 citation statements)
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“…The initial N concentration of 1.06% in larch litter was compatible with that measured at other Japanese larch forests (Osono et al, 2003;Son et al, 2004). Moreover, the C and N concentrations and a C:N ratio of broadleaf litter were within the range of those of other broadleaf species (Arunachalam et al, 1998;Wedderburn and Carter, 1999;Read and Lawrence, 2003). C concentration decreased in April for both broadleaf and larch litters.…”
Section: Seasonal Variation In Litter Co 2 Productionsupporting
confidence: 81%
See 1 more Smart Citation
“…The initial N concentration of 1.06% in larch litter was compatible with that measured at other Japanese larch forests (Osono et al, 2003;Son et al, 2004). Moreover, the C and N concentrations and a C:N ratio of broadleaf litter were within the range of those of other broadleaf species (Arunachalam et al, 1998;Wedderburn and Carter, 1999;Read and Lawrence, 2003). C concentration decreased in April for both broadleaf and larch litters.…”
Section: Seasonal Variation In Litter Co 2 Productionsupporting
confidence: 81%
“…As a result, the C:N ratio continued to decrease from May through September for broadleaf litter and from April through July for larch litter. The decrease in the C:N ratio with time was measured in many tree species at the early decomposition stage (Arunachalam et al, 1998;Wedderburn and Carter, 1999;Moro and Domingo, 2000). On the other hand, increasing C concentration and decreasing N concentration increased the C:N ratio from July through October in larch litter.…”
Section: Seasonal Variation In Litter Co 2 Productionmentioning
confidence: 98%
“…Vários fatores podem influenciar nas diferenças entre a serapilheira acumulada na floresta nos diferentes estádios do presente estudo, bem como com os outros tipos de floresta. Toda a dinâmica do material acumulado na superfície do solo é influenciada por fatores do ambiente, temperatura e umidade; pela qualidade inicial do material formador como, por exemplo, pelos componentes orgânicos; pelos macro e micronutrientes; pelos organismos do solo, como fauna, actomicetos e bactérias entre outros (O'CONNELL; SANKARAN, 1997;WEDDERBURN;CARTER, 1999 ).…”
Section: Methodsunclassified
“…Toda a dinâmica do material acumulado na superfície do solo é influenciada por fatores do ambiente, tais como temperatura e umidade; pela qualidade inicial do material formador como, por exemplo, pelos componentes orgânicos; pelos macronutrientes e micronutrientes; pelos organismos do solo, como fauna, actomicetos e bactérias entre outros (O'CONNELL; SANKARAN, 1997;WEDDERBURN;CARTER, 1999).…”
Section: Biomassaunclassified