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Similarly, maximum accumulation rates declined as carbon legacies increased (Figure 4d).
On average, the maximum accumulation rates occur in landscapes with mean ages around 10 years.
As carbon legacies increased to 30, 70, and 100%, maximum accumulation rates occurred at years 14, 18, and 19, respectively.
d) Effects of C legacies on the maximum accumulation rates (max NECB)), and the age at which this rate is reached (Age max NECB)).
A statistical fit to the data showed that this carbon accumulation is highly predictable, with maximum accumulation rates at around 9 years after the start of the successional process.
Similarly, maximum accumulation rates declined as carbon legacies increased.
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For amylopectin, the maximum accumulation rate, the time to reach the maximum accumulation rate, the accumulation duration, the average accumulation rate, and the initial growth power were greater in Ganken 5 than in Beiqing 6 and Kunlun 12.
The maximum starch accumulation rate, the time to the maximum accumulation rate, the accumulation duration, the average accumulation rate, and the initial growth power were greater in Kunlun 12 than in Beiqing 6.
For starch, the maximum accumulation rate, the average accumulation rate, and the initial growth power were all less in Ganken 5 than in Beiqing 6 and Kunlun 12.
For example, our simulations showed that carbon legacies control the period of time in which secondary forests act as carbon sources, the maximum accumulation rate that can be achieved during the entire successional process, and the time required to reach this maximum accumulation rate.
In the presence of legacies, secondary forests can act as carbon sources to the atmosphere, can decrease the maximum accumulation rate, and delay the time at which this maximum rate is reached.
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