Abstract
Fine roots play an important role in plant growth as well as carbon (C) and nutrient cycling in terrestrial ecosystems. Fine roots are important for understanding the contribution of forests to the global C cycle. Knowledge about this topic is still limited, especially regarding the effects of different forest management practices. This study investigated the seasonal dynamics of fine roots (<2 mm) in masson pine (P. massoniana) plantations for one year after low intensity thinning by using a sequential soil coring method. The fine roots showed pronounced seasonal dynamics, with a peak of fine root biomass (FRB) occurring in September. Significant differences were noted in the seasonal dynamics of FRB for the different diameter size sub-classes (≤0.5 mm, 0.5–1 mm and 1–2 mm); also FRB was inversely related to soil depth. Moreover, the FRB (≤0.5 mm and 0.5–1 mm except 1–2 mm) in the thinning plots was greater than that in the control only in the upper soil layer (0–10 cm). Furthermore, the FRB varied significantly with soil temperature, moisture and nutrients depended on the diameter sub-class considered. Significant differences in the soil temperature and moisture levels were noted between low-intensity thinned and control plots. Soil nutrient levels slightly decreased after low-intensity thinning. In addition, there was a more sensitive relationship between the very fine roots (diameter < 0.5 mm) and soil nutrients. Our results showed an influence of low-intensity thinning on the fine root dynamics with a different magnitude according to fine root diameter sub-classes. These results provide a theoretical basis to promote the benefits of C cycling in the management of P. massoniana forests.
Highlights
Forests are an important component of the global carbon (C) budget as a major C sink because they store approximately 80% of all terrestrial aboveground C and about 44% of all soil organicC [1,2,3]
The time at which the samples were obtained had a significant effect on the seasonal dynamics of the fine root biomass (FRB) in the ≤0.5 mm size sub-class at a depth of 0–20 cm in the thinned and control plots, but not at a depth of 20–30 cm. These results suggest that time was not the key factor affecting the seasonal dynamics of FRB in the ≤0.5 mm size sub-class
AK were positively, but not significantly, correlated with the FRB. These findings suggest that the seasonal dynamics of fine root (
Summary
Forests are an important component of the global carbon (C) budget as a major C sink because they store approximately 80% of all terrestrial aboveground C and about 44% of all soil organicC [1,2,3]. The roots of forest trees are a vital source of soil C [4,5,6], especially fine roots (i.e.,
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