Abstract

Forest planting is a common practice in semi-arid sandy land restoration, but problems may appear associated with forest age like higher soil water consumption that threatens restoration programā€™s success. This study quantified the distribution and variation of soil water storage in a Pinus sylvestris (P. sylvestris) plantation under various stand ages (20, 30, 40, 50 and 60 years) along 0ā€“1000 cm soil profile in the Mu Us sandy lands (North China). Results indicated that the 20-yr forests mainly consumed the soil water of the 0ā€“200 cm depth soil profile, the 30-yr and 40-yr forests mainly consumed the soil water of the depth of 0ā€“400 cm, whereas the oldest (50ā€“60-yr) pines mainly consumed the soil water located at the deepest soil profile (500ā€“700 cm). Variation of soil water storage (ā–³SWS) was decreased with stand ages, reaching the minimum value in the 30ā€“40-yr stands, and then gradually increased in the 50ā€“60-yr stands. The ā–³SWS was relatively uniform on the 50-yr and 60-yr stands. this pattern was associated with soil desiccation and soil-water depletion. The lower ā–³SWS indicated lower soil water storage which was associated with soil desiccation and soil-water depletion. These findings proved that planted forest gradually aggravated soil water consumption along the increasing forest age, caused a serious soil water deficit in the 200ā€“700 cm depth soil layer, which may be exceeding the water environmental carrying capacity. Therefore, we suggest that forest should be thinned on the periods with the highest ā–³SWS, which would maintain long-term forest sustainability by minimizing soil desiccation for planted forest management in semi-arid sandy lands.

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