期刊
SOIL SCIENCE AND PLANT NUTRITION
卷 47, 期 1, 页码 17-26出版社
JAPANESE SOC SOIL SCIENCE PLANT NUTRITION
DOI: 10.1080/00380768.2001.10408364
关键词
C-3 plant; C-4 plant; carbon turnover; natural C-13 abundance (delta C-13); soil organic carbon
The carbon content and natural C-13 abundance (delta C-13) of soil organic carbon were determined for Japanese cropland and nearby forest soils by continuous dow CN analysis with mass spectrometry. The delta C-13 values of organic carbon from cropland soils in the Hokkaido District ranged between -27 and -24 parts per thousand, suggesting that soil organic carbon originated mainly from C-3 plants, while the delta C-13 values from those in Main Island, Shikoku, and Kyushu Districts ranged between -25 and -17 parts per thousand, indicating that up to 70% of soil organic carbon originated from C-4 plants (presumably Miscanthus sinensis), The delta C-13 values of organic carbon from Imaichi and Tanegashima forest soils showed that carbon was largely of C-3 plant origin in the surface soils but in deeper horizons the values were strongly affected by the organic carbon of C-4 plant origin. Sugarcane cultivation for 36 y in Tanegashima cropland soils had resulted in the increase of the soil delta C-13 values to around -15 parts per thousand. In Shizuoka Prefecture, the delta C-13 values of soil organic carbon of non-volcanic ash Andosols under forests at Iwata and Makinohara were within the ranges of C-3 plant origin. The values in volcanic ash Andosols at Fuji indicated that the soil carbon in the surface horizons mainly originated from C-3 plants while that in deep soil horizons largely from C-4 plants. Tea cultivation for more than 40 y had led to a decrease of the delta C-13 values at Fuji by 2-4 parts per thousand. In the Miyako Island sugarcane fields, the delta C-13 values of the plow layers were apparently affected by sugarcane, a C-4 plant species, compared to the subsoils where a large fraction of carbon originated from C-3 forest plants. The shift from forest to sugarcane cultivation markedly decreased the carbon content and increased the delta C-13 values of soil organic carbon from -27--25 parts per thousand to -17--14 parts per thousand within 25 y.
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