Relationships between soil respiration (class="mathmlsrc">class="formulatext stixSupport mathImg" data-mathURL="/science?_ob=MathURL&_method=retrieve&_eid=1-s2.0-S0378112715002856&_mathId=si2.gif&_user=111111111&_pii=S0378112715002856&_rdoc=1&_issn=03781127&md5=2e403c96d94012271cb8898d64e02a47" title="Click to view the MathML source">RSclass="mathContainer hidden">class="mathCode">) and abiotic and biotic factors explored.
Apparent temperature response of soil respiration decreased by drought.
Annual soil respiration ranged from 12.0 to 13.9 Mg CO2 ha−1 year−1.
Temperature-normalized class="mathmlsrc">class="formulatext stixSupport mathImg" data-mathURL="/science?_ob=MathURL&_method=retrieve&_eid=1-s2.0-S0378112715002856&_mathId=si2.gif&_user=111111111&_pii=S0378112715002856&_rdoc=1&_issn=03781127&md5=2e403c96d94012271cb8898d64e02a47" title="Click to view the MathML source">RSclass="mathContainer hidden">class="mathCode"> related to proximity of trees and pine root biomass.