Aufsatz
Field measurements of the CO2 evolution rate under different crops during an irrigation cycle in a mountain oasis of Oman
Abstract
For millennia oasis agriculture has been the backbone of rural livelihood in the desertic Sultanate of Oman. However, little is known about the functioning of these oasis systems, in particular with respect to the C turnover. The objective was to determine the effects of crop, i.e. alfalfa, wheat and bare fallow on the CO2 evolution rate during an irrigation cycle in relation to changes in soil water content and soil temperature. The gravimetric soil water content decreased from initially 24% to approximately 16% within 7 days after irrigation. The mean CO2 evolution rates increased significantly in the order fallow
(27.4 mg C m^−2 h^−1) < wheat (45.5 mg C m^−2 h^−1) < alfalfa (97.5 mg C m^−2 h^−1). It can be calculated from these data that the CO2 evolution rate of the alfalfa root system was nearly four times higher than the corresponding rate in the wheat root system. The decline in CO2 evolution rate, especially during the first 4 days after irrigation, was significantly related to the decline in the gravimetric water content, with r = 0.70. CO2 evolution rate and soil temperature at 5 cm depth were negatively correlated (r = -0.56,n = 261) due to increasing soil temperature with decreasing gravimetric water content.
(27.4 mg C m^−2 h^−1) < wheat (45.5 mg C m^−2 h^−1) < alfalfa (97.5 mg C m^−2 h^−1). It can be calculated from these data that the CO2 evolution rate of the alfalfa root system was nearly four times higher than the corresponding rate in the wheat root system. The decline in CO2 evolution rate, especially during the first 4 days after irrigation, was significantly related to the decline in the gravimetric water content, with r = 0.70. CO2 evolution rate and soil temperature at 5 cm depth were negatively correlated (r = -0.56,n = 261) due to increasing soil temperature with decreasing gravimetric water content.
Citation
In: Applied soil ecology. Amsterdam : Elsevier. 25.2004, H. 1, S. 85-91Collections
Publikationen (Fachgebiet Ökologischer Pflanzenbau und Agrarökosystemforschung in den Tropen und Subtropen)Citation
@article{urn:nbn:de:hebis:34-2007051418170,
author={Wichern, Florian and Luedeling, Eike and Müller, Torsten and Jörgensen, Rainer Georg and Bürkert, Andreas},
title={Field measurements of the CO2 evolution rate under different crops during an irrigation cycle in a mountain oasis of Oman},
year={2004}
}
0500 Oax 0501 Text $btxt$2rdacontent 0502 Computermedien $bc$2rdacarrier 1100 2004$n2004 1500 1/eng 2050 ##0##urn:nbn:de:hebis:34-2007051418170 3000 Wichern, Florian 3010 Luedeling, Eike 3010 Müller, Torsten 3010 Jörgensen, Rainer Georg 3010 Bürkert, Andreas 4000 Field measurements of the CO2 evolution rate under different crops during an irrigation cycle in a mountain oasis of Oman / Wichern, Florian 4030 4060 Online-Ressource 4085 ##0##=u http://nbn-resolving.de/urn:nbn:de:hebis:34-2007051418170=x R 4204 \$dAufsatz 4170 7136 ##0##urn:nbn:de:hebis:34-2007051418170
2007-05-14T11:30:38Z 2007-05-14T11:30:38Z 2004 0929-1393 urn:nbn:de:hebis:34-2007051418170 http://hdl.handle.net/123456789/2007051418170 82544 bytes application/pdf eng Urheberrechtlich geschützt https://rightsstatements.org/page/InC/1.0/ Arid climate Soil respiration Sustainability 630 Field measurements of the CO2 evolution rate under different crops during an irrigation cycle in a mountain oasis of Oman Aufsatz For millennia oasis agriculture has been the backbone of rural livelihood in the desertic Sultanate of Oman. However, little is known about the functioning of these oasis systems, in particular with respect to the C turnover. The objective was to determine the effects of crop, i.e. alfalfa, wheat and bare fallow on the CO2 evolution rate during an irrigation cycle in relation to changes in soil water content and soil temperature. The gravimetric soil water content decreased from initially 24% to approximately 16% within 7 days after irrigation. The mean CO2 evolution rates increased significantly in the order fallow (27.4 mg C m^−2 h^−1) < wheat (45.5 mg C m^−2 h^−1) < alfalfa (97.5 mg C m^−2 h^−1). It can be calculated from these data that the CO2 evolution rate of the alfalfa root system was nearly four times higher than the corresponding rate in the wheat root system. The decline in CO2 evolution rate, especially during the first 4 days after irrigation, was significantly related to the decline in the gravimetric water content, with r = 0.70. CO2 evolution rate and soil temperature at 5 cm depth were negatively correlated (r = -0.56,n = 261) due to increasing soil temperature with decreasing gravimetric water content. open access In: Applied soil ecology. Amsterdam : Elsevier. 25.2004, H. 1, S. 85-91 Wichern, Florian Luedeling, Eike Müller, Torsten Jörgensen, Rainer Georg Bürkert, Andreas The original publication is available at www.elsevier.com
The following license files are associated with this item: