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• W2905841207 abstract "Plantation development stage (forest age sequence) influences environmental conditions and litter inputs, which can modify labile C and N pools. Changes in labile C and N pools during stand development could vary considerably with soil parent material. However, empirical evidence is scarce regarding the extent of interactive effects between parent material and stand development stage on labile C and N pools in plantations of Chinese fir (Cunninghamia lanceolata (Lamb.) Hook.), the dominant plantation tree in southern China. We examined the concentrations of soil labile C and N (dissolved organic carbon, DOC, dissolved organic nitrogen, DON, dissolved inorganic nitrogen, DIN, microbial biomass carbon, Cmic, microbial biomass nitrogen, Nmic) and basic soil properties within a soil depth of 100 cm for three stand development stages (young, middle-aged and mature) of Chinese fir plantations grown on soils derived from granite or siltstone. The parent material influenced the responses of the DON, DIN and Nmic pools to stand development stage, whereas no interaction effect of parent material and stand on the Cmic and DOC pools was observed. The parent material had a clear effect on the standing pools of labile C and N. Siltstone soils tended to have greater pool sizes of DOC, DON, DIN, and Nmic and greater ratios of Cmic/total carbon (TC) and Nmic/total nitrogen (TN). The stand development stage did not affect the DOC, Cmic and Cmic/TC ratio. The mineral N and Nmic pools increased significantly and the DON and DON/TN ratio declined sharply from young to middle-aged stands in both soil type. The changes in the DON, DIN and Nmic pools and the Nmic/TN ratio from middle-aged to mature stands depend on the parent material. The concentrations of DOC, DON, DIN, Cmic and Nmic were positively correlated with multiple soil parameters, such as the TC, TN, C/N ratio, water-stable aggregates (WSA), and water content, but negatively correlated with the bulk density (BD). DOC, DON, Cmic and Nmic significantly decreased with soil depth, but the extent of the decrease in DOC and DON was greater in course-textured granite soils. Overall, the turnover rates of the labile C pools are higher in the siltstone soils where internal N cycling during a traditional rotation ~25 years maintain the supply of mineral N and improve N incorporation into microbial biomass. These results highlight the need to identify soil physicochemical properties before afforestation. The rotation length and N fertilizer application in Chinese fir plantations should be adjusted based on the soil parent material." @default.
• W2905841207 created "2019-01-01" @default.
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• W2905841207 date "2019-03-01" @default.
• W2905841207 modified "2023-10-16" @default.
• W2905841207 title "Soil parent material and stand development stage effects on labile soil C and N pools in Chinese fir plantations" @default.
• W2905841207 cites W1962071678 @default.
• W2905841207 cites W1964122210 @default.
• W2905841207 cites W1970782132 @default.
• W2905841207 cites W1971229566 @default.
• W2905841207 cites W1978146995 @default.
• W2905841207 cites W1980103489 @default.
• W2905841207 cites W1984248590 @default.
• W2905841207 cites W1984768452 @default.
• W2905841207 cites W1989577118 @default.
• W2905841207 cites W1995548542 @default.
• W2905841207 cites W1996387759 @default.
• W2905841207 cites W1996440470 @default.
• W2905841207 cites W2000892282 @default.
• W2905841207 cites W2005306137 @default.
• W2905841207 cites W2009673336 @default.
• W2905841207 cites W2009781485 @default.
• W2905841207 cites W2010094899 @default.
• W2905841207 cites W2010710061 @default.
• W2905841207 cites W2010961248 @default.
• W2905841207 cites W2029718117 @default.
• W2905841207 cites W2030690628 @default.
• W2905841207 cites W2030707978 @default.
• W2905841207 cites W2037138355 @default.
• W2905841207 cites W2037699113 @default.
• W2905841207 cites W2040931818 @default.
• W2905841207 cites W2043801120 @default.
• W2905841207 cites W2047103392 @default.
• W2905841207 cites W2050077059 @default.
• W2905841207 cites W2054532641 @default.
• W2905841207 cites W2055592323 @default.
• W2905841207 cites W2064164498 @default.
• W2905841207 cites W2066433875 @default.
• W2905841207 cites W2068248597 @default.
• W2905841207 cites W2068667325 @default.
• W2905841207 cites W2072627116 @default.
• W2905841207 cites W2074374419 @default.
• W2905841207 cites W2076493894 @default.
• W2905841207 cites W2076626791 @default.
• W2905841207 cites W2090083053 @default.
• W2905841207 cites W2100070262 @default.
• W2905841207 cites W2101772716 @default.
• W2905841207 cites W2102819180 @default.
• W2905841207 cites W2104191557 @default.
• W2905841207 cites W2104486225 @default.
• W2905841207 cites W2108823744 @default.
• W2905841207 cites W2114962172 @default.
• W2905841207 cites W2115232352 @default.
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• W2905841207 cites W2124721818 @default.
• W2905841207 cites W2128067656 @default.
• W2905841207 cites W2135136903 @default.
• W2905841207 cites W2139429225 @default.
• W2905841207 cites W2139610873 @default.
• W2905841207 cites W2146606951 @default.
• W2905841207 cites W2150345087 @default.
• W2905841207 cites W2158243811 @default.
• W2905841207 cites W2161463470 @default.
• W2905841207 cites W2163875956 @default.
• W2905841207 cites W2166915931 @default.
• W2905841207 cites W2338646640 @default.
• W2905841207 cites W2398144804 @default.
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• W2905841207 doi "https://doi.org/10.1016/j.geoderma.2018.11.050" @default.
• W2905841207 hasPublicationYear "2019" @default.
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