Soil organic matter dynamics in lands continuously cultivated with maize [[Zea mays] and soybean [Glycine max] in Heilongjiang Province, Northeast China: Estimation from natural 13C abundance
2006
Wang, G.(Chinese Academy of Sciences, Harbin (China)) | Han, X. | Nakayama, N. | Watanabe, T. | Watanabe, A. | Kimura, M.
Northeast China is the main production area of maize and soybean in China. In the present study, the rates of decomposition and replacement of soil organic carbon (SOC) were estimated using the soil inventory collected since 1991 from long-term maize and soybean cultivation plots in Heilongjiang Province, Northeast China, to evaluate the sustainability of the present cultivation system. The total carbon (C) content in soil was stable without any significant changes in the plots (approximately 28.5 g C /kg). The deltasup(13)C value of soil organic matter under continuous maize cultivation increased linearly with an annual increment of 0.07 permille, from -23,9 permille in 1991, which indicated that approximately 13% of the initial SOC was decomposed during the 13-year period of maize cultivation, with a half-life of 65 years. Slow decomposition of SOC was considered to result from the low annual mean temperature (1.5 deg C) and long freezing period (170-180 days /year) in the study area. In contrast, the amount of organic C derived from maize increased in the soil with a very slow annual increment of 0.17g C /kg, probably because of the removal of all the plant residues from the plots. Based on the soil organic matter dynamics observed in the study plots, intentional recycling/maintenance of plant residues was proposed as a way of increasing soil fertility in maize or soybean cultivation.
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