水保所知识产出(1956---)知识库

Afforestation on abandoned cropland has great potential to increase soil organic carbon (OC) and nitrogen (N).
Identifying the effect of afforestation on mineralization of OC and N as well as their temperature sensitivity at
large spatial and temporal scales is essential to understand soil OC and N dynamics. In this study, we measured
mineralization of soil OC and N at standard temperatures (15 and 25 ◦ C) by laboratory incubation, and calculated
their temperature sensitivity (Q 10 ). Soil samples were collected from cropland (0 years, selected as a control) and
adjacent woodlands with different afforestation age (10, 20 and 30 years) at five sites from north to south on
China’s Loess Plateau. The objectives were to understand how long-term afforestation affects OC and N
mineralization and their Q 10 and whether such effects depend on afforestation age and soil texture. The results
showed that afforestation increased OC and N mineralization, but this effect was not affected by afforestation age
(10–30 years). The Q 10 of OC and N mineralization increased in the first 10 years of afforestation but decreased
in the late stage. Furthermore, the increases of OC and N mineralization by afforestation were higher at sites with
fine-textured soils than those at sites with coarse-textured soils. However, the Q 10 increased at sites with a
relatively high sand content but decreased or remained unchanged at sites with a relatively high clay content.
The changes in OC and N mineralization and their Q 10 were related to soil OC and N contents, pH and clay
content. Overall, we concluded that long-term afforestation would contribute to the stability of soil OC and N in
afforested ecosystems. Soil texture is an important factor controlling OC and N mineralization and their Q 10 , and
should be considered when predicting soil OC and N dynamics in response to temperature change in different
landscapes.