Soil carbon (C) in three Ginkgo (Ginkgo biloba L.) agroforestry systems, afforestation (Ginkgo alone; G), and an agricultural cropping system were compared over a five-year period. The agroforestry systems were Ginkgo + Wheat (Triticum aestivum L.) + Peanut (Arachis hypogaea L.; GWP); Ginkgo + Mulberry (Morus alba L.; GM); and Ginkgo + Rapa (Brassica napus L.) + Peanut (GRP). The agricultural system consisted of wheat and peanut (WP). Total soil carbon (TSC), soil organic (SOC) and inorganic carbon (SIC), and the pools of five SOC chemical fractions were measured. TSC and SOC were always lower under WP than the G-based planting systems, and TSC in the latter increased significantly across years in the top 20 cm. Stocks of SIC under WP were significantly greater than the G-based systems, whereas SOC fractions tended to be lower. Most fractions increased across years but not in WP.

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hypogaea l gwp soil organic soc inorganic carbon

Guibin Wang,Clive Welham,Chaonian Feng,Lei Chen,Fuliang Cao,.Enhanced Soil Carbon Storage under Agroforestry and Afforestation in Subtropical China. 6 (7),.

Guibin Wang,Clive Welham,Chaonian Feng,Lei Chen,Fuliang Cao,"Enhanced Soil Carbon Storage under Agroforestry and Afforestation in Subtropical China" 6

Guibin Wang,Clive Welham,Chaonian Feng,Lei Chen,Fuliang Cao,"Enhanced Soil Carbon Storage under Agroforestry and Afforestation in Subtropical China"