2016
DOI: 10.3390/f7120309
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Heterotrophic Soil Respiration Affected by Compound Fertilizer Types in Red Pine (Pinus densiflora S. et Z.) Stands of Korea

Abstract: This study was conducted to evaluate the effects of fertilizer application on heterotrophic soil respiration (Rh) in soil respiration (Rs) components in red pine stands. Two types of fertilizer (N 3 P 4 K 1 = 113:150:37 kg·ha −1 ·year −1 ; P 4 K 1 = 150:37 kg·ha −1 ·year −1 ) were applied manually on the forest floor for two years. Rs and Rh rates were monitored from April 2011 to March 2013. Mean Rs and Rh rates were not significantly affected by fertilizer applications. However, Rh in the second year followi… Show more

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Cited by 5 publications
(2 citation statements)
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“…The samples during this preliminary study were collected in June and August, but due to the low number of samples (and lack of in-field replication that reflects modern statistical methods), we could not assess the intra-annual variation in nitrification potential, nitrifier communities, or the edaphic drivers. Biotic factors, such as microbial enzyme potential and community structure, vary significantly spatiotemporally (8,114,115). Particularly, Nmineralization (116) and urease enzyme activity (117) increase with temperature, resulting in late-season pulses in these enzyme activities.…”
Section: Study Limitationsmentioning
confidence: 99%
“…The samples during this preliminary study were collected in June and August, but due to the low number of samples (and lack of in-field replication that reflects modern statistical methods), we could not assess the intra-annual variation in nitrification potential, nitrifier communities, or the edaphic drivers. Biotic factors, such as microbial enzyme potential and community structure, vary significantly spatiotemporally (8,114,115). Particularly, Nmineralization (116) and urease enzyme activity (117) increase with temperature, resulting in late-season pulses in these enzyme activities.…”
Section: Study Limitationsmentioning
confidence: 99%
“…Soil C fluxes were characterized by determining the total soil CO 2 efflux and heterotrophic respiration, whereas soil N fluxes were characterized by determining the net mineralization and nitrification rates using an in situ incubation method. Total soil CO 2 efflux was separated into root- and heterotrophic respiration using a trench method 59 . A root exclusion barrier (50 cm diameter, 30 cm depth, PVC) was installed in each plot, 4 weeks before the treatments were initiated.…”
Section: Methodsmentioning
confidence: 99%