nstantaneous and historical temperature effects on a-pinene
Heating induced changes in
mineral nitrogen and organic carbon
in relation with temperature
and time
Author Details
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HuseyinBarisTecimen (Corresponding author)
IstanbulUniversity, Faculty of Forestry, Soil Science and Ecology Department -
34473, Bahcekoy,
Istanbul, Turkey
e-mail:
baristecimen@gmail.com
OrhanSevgi
IstanbulUniversity, Faculty of Forestry, Soil Science and Ecology Department -
34473, Bahcekoy,
Istanbul, Turkey
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Publication Data
Paper received:
05
December 2010
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Revised
received:
27
April 2010
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Accepted:
12 May 2010
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Abstract
Heating effects on carbon
and mineral nitrogen contents of soils within different land use types were
investigated in this study. With this intention we collected soil samples
from 3 different land use types which are abandoned agricultural lands (AAL),
shrub land (SL) and Oak forest
land (OFL) and are in neighborhood with each other. The sampling was made at
mid-summer to provide a better correspondence between factual burning
conditions as well. Soils are slightly acidic (pH between
4.60-5.72) and sandy, sandy loamy textured. At the study site the
vegetation type is pasture at AAL, Cystus
and Rubus sp. dominated shrubs at SL and
mixture of Oak species such as Quercuspetrea, Q. robur, Q. cerris and Q. frainettoat
OFL. The results we found revealed that heating temperature has more
remarkable effect on C losses and soil NH4+-N
re-mineralization and losses of NH4+-N. Besides we
could not detect remarkable differences between total N and NO3- amounts. Heating time
created significant differences between NH4+-N amounts
for different land use types where SL soils showed significant difference for
all temperature levels. Heating soils at 100oC created only slight
differences at C and NH4+-N budgets but heating at 200oC
caused to striking results at NH4+-N budgets and
heating at 350oC led to only slight increase at NH4+-N
budget. As the temperature increased the C loss also increased linearly.