FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2892541284> ?p ?o ?g. }

• W2892541284 endingPage "61" @default.
• W2892541284 startingPage "52" @default.
• W2892541284 abstract "Soil heterotrophic respiration was profoundly correlated with the decomposition of soil organic carbon and the global carbon balance. It was liable to be affected by temperature and carbon substrate availability. To investigate the effects of different carbon substrate inputs on organic carbon decomposition and the temperature sensitivity of soil heterotrophic respiration along the forest stand ages, we sampled surface soils (0–20 cm) from three Quercus Mongolica forest stands (20, 30 and 40 years old) in Northeast China. The microcosms were established to incubate the soil under three carbon substrate treatments (glucose, amylopectin, and the combination of glucose and amylopectin) at 13, 23, and 33 °C, respectively. The carbon substrates were 320 μmol g−1 and 40 μmol g−1 fresh soil for glucose and amylopectin, respectively. The combined treatment was 160 μmol glucose g−1 and 20 μmol amylopectin g−1 fresh soil. The results showed that rates of basal respiration (BR), substrate-induced respiration (SIR), and specific growth rate (SGR) significantly increased with the increasing forest ages. After the addition of carbon substrates, the stimulation effects of SIR and SGR were higher at 23 °C than 13 °C and 33 °C, especially the addition of amylopectin. The Q10 values of SIR were lower after the addition of glucose than those of amylopectin at lower temperature intervals (13–23 °C), but higher at higher temperatures (23–33 °C). The Q10 linearly increased with increasing rates of substrate availability. The Q10 values of SIR stimulated by amylopectin were higher at lower temperature intervals (13–23 °C), suggesting the responses of Q10 were not only adjusted by carbon substrates but also the ranges of temperature change. The exogenous stable organic carbon inputs greatly increased the Q10 values of soil heterotrophic respiration in the older forest stands. These results indicated that the decomposition of stable carbon substrate will be more sensitivity to temperature in boreal successional Quercus Mongolica forest." @default.
• W2892541284 created "2018-10-05" @default.
• W2892541284 creator A5001945428 @default.
• W2892541284 creator A5002260375 @default.
• W2892541284 creator A5011305234 @default.
• W2892541284 creator A5036995131 @default.
• W2892541284 creator A5040258136 @default.
• W2892541284 creator A5064735625 @default.
• W2892541284 date "2019-01-01" @default.
• W2892541284 modified "2023-10-14" @default.
• W2892541284 title "Temperature sensitivity of soil heterotrophic respiration is altered by carbon substrate along the development of Quercus Mongolica forest in northeast China" @default.
• W2892541284 cites W1685833191 @default.
• W2892541284 cites W1898766722 @default.
• W2892541284 cites W1918894213 @default.
• W2892541284 cites W1964589705 @default.
• W2892541284 cites W1965248862 @default.
• W2892541284 cites W1965578568 @default.
• W2892541284 cites W1969069662 @default.
• W2892541284 cites W1969713080 @default.
• W2892541284 cites W1979017704 @default.
• W2892541284 cites W1979534624 @default.
• W2892541284 cites W1984412649 @default.
• W2892541284 cites W1991514081 @default.
• W2892541284 cites W1993253346 @default.
• W2892541284 cites W1996725834 @default.
• W2892541284 cites W2003781647 @default.
• W2892541284 cites W2008296782 @default.
• W2892541284 cites W2015710670 @default.
• W2892541284 cites W2018318056 @default.
• W2892541284 cites W2024340952 @default.
• W2892541284 cites W2035017164 @default.
• W2892541284 cites W2035614014 @default.
• W2892541284 cites W2035748504 @default.
• W2892541284 cites W2036025427 @default.
• W2892541284 cites W2036085139 @default.
• W2892541284 cites W2039663712 @default.
• W2892541284 cites W2041570407 @default.
• W2892541284 cites W2043622617 @default.
• W2892541284 cites W2044415600 @default.
• W2892541284 cites W2049207331 @default.
• W2892541284 cites W2050130013 @default.
• W2892541284 cites W2050986529 @default.
• W2892541284 cites W2051707883 @default.
• W2892541284 cites W2051931181 @default.
• W2892541284 cites W2054375821 @default.
• W2892541284 cites W2055741320 @default.
• W2892541284 cites W2057413126 @default.
• W2892541284 cites W2059475318 @default.
• W2892541284 cites W2064219231 @default.
• W2892541284 cites W2075925671 @default.
• W2892541284 cites W2076357620 @default.
• W2892541284 cites W2083857556 @default.
• W2892541284 cites W2087474788 @default.
• W2892541284 cites W2090447760 @default.
• W2892541284 cites W2090602773 @default.
• W2892541284 cites W2099586679 @default.
• W2892541284 cites W2100290432 @default.
• W2892541284 cites W2104380608 @default.
• W2892541284 cites W2105961364 @default.
• W2892541284 cites W2106458285 @default.
• W2892541284 cites W2107839033 @default.
• W2892541284 cites W2109937711 @default.
• W2892541284 cites W2119968371 @default.
• W2892541284 cites W2120721798 @default.
• W2892541284 cites W2120900106 @default.
• W2892541284 cites W2123567531 @default.
• W2892541284 cites W2134744919 @default.
• W2892541284 cites W2136009149 @default.
• W2892541284 cites W2136820276 @default.
• W2892541284 cites W2138540827 @default.
• W2892541284 cites W2140014421 @default.
• W2892541284 cites W2141350212 @default.
• W2892541284 cites W2151305472 @default.
• W2892541284 cites W2160489903 @default.
• W2892541284 cites W2161955723 @default.
• W2892541284 cites W2164586753 @default.
• W2892541284 cites W2171580662 @default.
• W2892541284 cites W2172084595 @default.
• W2892541284 cites W2229551426 @default.
• W2892541284 cites W2497991264 @default.
• W2892541284 cites W2546822929 @default.
• W2892541284 cites W2550788627 @default.
• W2892541284 cites W2696995113 @default.
• W2892541284 cites W2733793964 @default.
• W2892541284 cites W2754012948 @default.
• W2892541284 cites W2767698430 @default.
• W2892541284 cites W4231864045 @default.
• W2892541284 cites W4239333307 @default.
• W2892541284 cites W4246797971 @default.
• W2892541284 doi "https://doi.org/10.1016/j.apsoil.2018.09.010" @default.
• W2892541284 hasPublicationYear "2019" @default.
• W2892541284 type Work @default.
• W2892541284 sameAs 2892541284 @default.
• W2892541284 citedByCount "14" @default.
• W2892541284 countsByYear W28925412842020 @default.
• W2892541284 countsByYear W28925412842021 @default.
• W2892541284 countsByYear W28925412842022 @default.
• W2892541284 countsByYear W28925412842023 @default.

• next