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Transformations of mineral nitrogen applied to peat soil during sequential oxic/anoxic cycling
ID
Pal, Levin
(
Avtor
),
ID
Stres, Blaž
(
Avtor
),
ID
Danevčič, Tjaša
(
Avtor
),
ID
Leskovec, Simona
(
Avtor
),
ID
Mandić-Mulec, Ines
(
Avtor
)
URL - Predstavitvena datoteka, za dostop obiščite
http://dx.doi.org/10.1016/j.soilbio.2010.03.013
Galerija slik
Izvleček
Shifts in oxic and anoxic conditions in soil are most frequently caused by water table fluctuations, heavy rain, snowmelt or flooding, with potentially significant impacts on microbial processes and the ability of soils to convert mineral nitrogen gases efficiently. The impact of oxic/anoxic cycles on nitrogen transformation rates was therefore explored in the upper layer (0-30 cm) of partially degraded peat soil. We hypothesized that high denitrification potential would be conserved due to the high organic matter content of this soil. Mineral nitrogen was applied to approximately 1-cm deep layers of homogenized soil in microcosms, with no external source of readily degradable carbon. Microcosms were subjected to three cycles, each consisting of an oxic phase of 8-11 days and an anoxic phase of 21-28 days. Approximately 2% of the ammonium load was lost through ammonia volatilization during oxic phases and the remainder was nitrified. The accumulated nitrate decreased soil ph from 8.0 to 6.8 before its transformation through denitrification. Nitrification and denitrification rates during the three oxic/anoxic cycles (approximately three months) were.29-3.2 kg N ha [up]-1 and 1.0-2.3 kg N ha[up]-1, respectively. Extrapolation of these values to 30-cm deep soil layers gave rates that were sufficient for complete transformation of at least 1700 kg N ha [up]-1 of ammonium to nitrogen gases, which is ten-fold greater than the annual nitrogen application of 170 kg N ha[up]-1 permitted by the European directive. Denitrification rates decreased linearly during the three cycles (from 36+-2 to 16+-ug N g [up-1] d [up]-1 drysoil projecting cessation of denitrification activity and Co2 production during the fifth cycle. Storage of peat at 4oC most probably allowed slow degradation of organic matter that was completely oxidized to Co2 after the soil was exposed to higher temeprature (28oC). Storage of soil for one year did not affect nitrification rate, but reduced denitrifation rate, unless soilwas amended with a readily degradable carbon source. The data suggest thatthe high carbon content of this soil, it cannot sustain transformations ofhigh N loads to nitrogen gases for prolonged periods without amendment with readily available carbon.
Jezik:
Angleški jezik
Vrsta gradiva:
Delo ni kategorizirano
Tipologija:
1.01 - Izvirni znanstveni članek
Organizacija:
BF - Biotehniška fakulteta
Leto izida:
2010
Št. strani:
Str. 1338-1346
Številčenje:
Vol. 42, Issue 8
PID:
20.500.12556/RUL-83231
UDK:
502
ISSN pri članku:
0038-0717
DOI:
10.1016/j.soilbio.2010.03.013
COBISS.SI-ID:
2619272
Datum objave v RUL:
18.08.2016
Število ogledov:
1993
Število prenosov:
289
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Objavi na:
Gradivo je del revije
Naslov:
Soil biology & biochemistry
Skrajšan naslov:
Soil biol. biochem.
Založnik:
Pergamon Press
ISSN:
0038-0717
COBISS.SI-ID:
5224199
Sekundarni jezik
Jezik:
Slovenski jezik
Ključne besede:
varstvo okolja
,
tla
,
šota
,
dušik
,
kroženje dušika
,
nitrifikacija
,
dentrifikacija
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