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Cover crop rotations in no-till system: short-term CO

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Academic year: 2019

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Table 1 – Selected chemical characteristics of the crops in the crop  rotation systems.
Figure 2 – CO 2  flux in g m –2  h –1  (A), soil temperature in °C (B), and  soil moisture in m 3  m –3  (C), at 1, 2, 3, 8, 15, 30, 60, 90 and 120  days after sowing of soybean in accordance with different crop  sequences in the Typic Rhodudalf soil
Figure 4 – Pearson correlation (*p < 0.05) between the CO 2  flux  (g m –2  h –1 ) and soil moisture (m 3  m –3 ) (A) and soil temperature (°C)  (B) in the Typic Rhodudalf and the Rhodic Hapludox.
Table 2 – Accumulated C-CO 2  emissions, soybean grain yield, and  relative C-CO 2  emissions in the Typic Rhodudalf soil.
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