Soil Gaseous Emissions and Partial C and N Balances of Small-Scale Farmer Fields in a River Oasis of Western Mongolia

dc.date.accessioned2019-09-10T13:24:37Z
dc.date.available2019-09-10T13:24:37Z
dc.date.issued2019-06-18
dc.description.sponsorshipGefördert durch den Publikationsfonds der Universität Kassel
dc.identifierdoi:10.17170/kobra-20190910678
dc.identifier.urihttp://hdl.handle.net/123456789/11308
dc.language.isoeng
dc.relation.doidoi:10.3390/su11123362
dc.rightsUrheberrechtlich geschützt
dc.rights.urihttps://rightsstatements.org/page/InC/1.0/
dc.subjectammoniaeng
dc.subjectcarbon dioxideeng
dc.subjectcarbon losseseng
dc.subjectclosed chamber systemeng
dc.subjectMongolian Altai Mountainseng
dc.subjectnitrogen losseseng
dc.subjectnitrous oxideeng
dc.subjectphoto-acoustic multi-gas monitoreng
dc.subjectsoil fertilityeng
dc.subject.ddc630
dc.titleSoil Gaseous Emissions and Partial C and N Balances of Small-Scale Farmer Fields in a River Oasis of Western Mongoliaeng
dc.typeAufsatz
dc.type.versionpublishedVersion
dcterms.abstractDuring the last decades, Mongolian river oases were subjected to an expansion of farmland. Such intensification triggers substantial gaseous carbon (C) and nitrogen (N) losses that may aggravate disequilibria in the soil surface balances of agricultural plots. This study aims to quantify such losses, and assess the implications of these emissions against the background of calculated partial C and N balances. To this end, CO2, NH3, and N2O soil emissions from carrot, hay, and rye plots were measured by a portable dynamic closed chamber system connected to a photoacoustic multi-gas analyzer in six farms of the Mongolian river oasis Bulgan sum center. Average C and N flux rates (1313 g CO2-C ha−1 h−1 to 1774 g CO2-C ha−1 h−1; 2.4 g NH3-N ha−1 h−1 to 3.3 g NH3-N ha−1 h−1; 0.7 g N2O-N ha−1 h−1 to 1.1 g N2O-N ha−1 h−1) and cumulative emissions (3506 kg C ha−1 season−1 to 4514 kg C ha−1 season−1; 7.4 kg N ha−1 season−1 to 10.9 kg N ha−1 season−1) were relatively low compared to those of other agroecosystems, but represented a substantial pathway of losses (86% of total C inputs; 21% of total N inputs). All C and N balances were negative (−1082 kg C ha−1 season−1 to −1606 kg C ha−1 season−1; −27 kg N ha−1 season−1 to −65 kg N ha−1 season−1). To reduce these disequilibria, application of external inputs may need to be intensified whereby such amendments should be incorporated into soil to minimize gaseous emissions.eng
dcterms.accessRightsopen access
dcterms.creatorJordan, Greta
dcterms.creatorGoenster-Jordan, Sven
dcterms.creatorUlziisuren, Baigal
dcterms.creatorBuerkert, Andreas
dcterms.source.identifierISSN 2071-1050
dcterms.source.issueIssue 12
dcterms.source.journalSustainabilityeng
dcterms.source.pageinfo3362
dcterms.source.volumeVolume 11

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