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Titel |
The effect of cultivation practices on soil - atmosphere carbon cycle under arid climate conditions |
VerfasserIn |
David Lifschitz, Marcelo Sternberg, David Bonfil, Eyal Ben-Dor, Gil Eshel |
Konferenz |
EGU General Assembly 2010
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Medientyp |
Artikel
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Sprache |
Englisch
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Digitales Dokument |
PDF |
Erschienen |
In: GRA - Volume 12 (2010) |
Datensatznummer |
250039958
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Zusammenfassung |
The soil – atmosphere carbon cycle was studied under arid climate conditions, in relation to
crop management. Management included different tillage (Conventional vs. No Tillage, CT
vs. NT respectively) and fertilization (nitrogen and phosphorus application vs. unfertilized)
practices, in a continuous (winter) wheat field, for two growing seasons (2007-08 and
2008-09).
The NT practice was characterized by higher CO2 effluxes than the CT during the
growing season. In turn, the CT practice had higher pCO2 throughout the soil profile to a
depth of 2m. This could be explained partially by a physical crust formation due to
raindrop impact, emerging on the bare soil, mostly in the CT practice. The crust
serves as a barrier for gas exchange (soil aeration) and in addition, also reduces
rainfall infiltration, and all together harms the growing potential (the NT practice
yielded higher plant biomass). Fertilization application had no apparent effect on the
CO2 effluxes or the pCO2, but had a significant effect on the yield of the plant
biomass.
The NT practice had also higher amounts of soil organic Carbon, (SOC) mainly in the
surface layer, and soil inorganic Carbon (SIC) to a depth of 2m. This is attributed
to straw mulch application for the former and better gas and water conductivity
(that initiates carbonate dissolution – precipitation cycles) for the latter, which is a
much more dominant factor in arid area soils. The stable carbon isotope analysis
(δ13C) values for the total Carbon (TC), SOC and SIC results show that the NT
practice generates higher amounts of pedogenic carbonates also, and in general is
clearly superior over CT in almost every aspect in the soil – atmosphere C cycle. |
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