Web of Science: Soil respiration and controls in warmer winter: A snow manipulation study in postfire and undisturbed black pine forests
dc.contributor.author | Pacaldo, R.S. | |
dc.contributor.author | Aydin, M. | |
dc.contributor.author | Amarille, R.K. | |
dc.date.accessioned | 2024-03-27T10:48:56Z | |
dc.date.available | 2024-03-27T10:48:56Z | |
dc.date.issued | 2024.01.01 | |
dc.description.abstract | Climate change impacts drive warmer winters, reduced snowfall, and forest fires. In 2020, a wildfire scorched about 1508 hectares of black pine (Pinus nigra Arnold) forests in T & uuml;rkiye. Whether the combined effects of lack of snow and forest fires significantly alter winter soil respiration (R-s) and soil temperature remains poorly understood. A field experiment was conducted in the postfire and undisturbed black pine forests during the winter to quantify R-s rates as affected by lack of snow and forest fire. We applied four treatments: snow-exclusion postfire (SEPF), snow postfire (SPF), snow-exclusion-undisturbed forest (SEUF), and snow undisturbed forest (SUF). The SEPF exhibited the significantly lowest mean R-s rates (0.71 mu mol m(-2) s(-1)) compared to the SPF (1.02 mu mol m(-2) s(-1)), SEUF (1.44 mu mol m(-2) s(-1)), and SUF (1.48 mu mol m(-2) s(-1)). The R-s also showed significant variations with time (p < .0001). However, treatments and time revealed no statistically significant interaction effects (p = .6801). Total winter R-s (January-March) ranged from 4.47 to 4.59 Mt CO2 ha(-1) in the undisturbed forest and 2.20 to 3.16 Mt CO2 ha(-2) in the postfire site. The R-s showed a significantly positive relationship (p < .0001) with the soil (0.59) and air (0.46) temperatures and a significantly negative relationship (p = .0017) with the soil moisture (-0.20) at the 5 cm depth. In contrast, the R-s indicated a negative but not statistically significant relationship (p = .0932) with the soil moisture (-0.16) at the 10 cm soil depth. The combined effects of lack of snow and forest fire significantly decreased R-s, thus conserving the soil's organic carbon stocks and reducing the CO2 contribution to the atmosphere. In contrast, a warmer winter significantly increased R-s rates in the undisturbed forest, suggesting an acceleration of soil organic carbon losses and providing positive feedback to climate change. | |
dc.identifier.doi | 10.1002/ece3.11075 | |
dc.identifier.endpage | ||
dc.identifier.issn | 2045-7758 | |
dc.identifier.issue | 3 | |
dc.identifier.startpage | ||
dc.identifier.uri | https://www.webofscience.com/api/gateway?GWVersion=2&SrcApp=dspace_ku&SrcAuth=WosAPI&KeyUT=WOS:001180490000001&DestLinkType=FullRecord&DestApp=WOS_CPL | |
dc.identifier.uri | https://hdl.handle.net/20.500.12597/33025 | |
dc.identifier.volume | 14 | |
dc.identifier.wos | 001180490000001 | |
dc.language.iso | en | |
dc.relation.ispartof | ECOLOGY AND EVOLUTION | |
dc.rights | info:eu-repo/semantics/openAccess | |
dc.subject | air temperature | |
dc.subject | climate change | |
dc.subject | freeze-thaw | |
dc.subject | soil moisture | |
dc.subject | soil temperature | |
dc.subject | wildfire | |
dc.title | Soil respiration and controls in warmer winter: A snow manipulation study in postfire and undisturbed black pine forests | |
dc.type | Article | |
dspace.entity.type | Wos |