Wang Yi-Hao, Wang Yan-Hui, Li Zhen-Hua, Yu Peng-Tao, Xiong Wei, Hao Jia, Duan Jian
State Forestry Administration Key Laboratory of Forest Ecology and Environment, Institute of Forest Ecology, Environment and Protection, Chinese Academy of Forestry, Beijing 100091, China.
Ying Yong Sheng Tai Xue Bao. 2012 Oct;23(10):2632-40.
From March 2009 to November 2011, an investigation was conducted on the spatiotemporal variation of soil moisture and its effects on the needle-fall in Masson pine (Pinus massoniana) forests in acid rain region of Chongqing, Southeast China, with the corresponding soil moisture thresholds determined. No matter the annual precipitation was abundant, normal or less than average, the seasonal variation of soil moisture in the forests could be obviously divided into four periods, i.e., sufficient (before May), descending (from June to July), drought (from August to September), and recovering (from October to November). With increasing soil depth, the soil moisture content increased after an initial decrease, but the difference of the soil moisture content among different soil layers decreased with decreasing annual precipitation. The amount of monthly needle-fall in the forests in growth season was significantly correlated with the water storage in root zone (0-60 cm soil layer), especially in the main root zone (20-50 cm soil layer). Soil field capacity (or capillary porosity) and 82% of field capacity (or 80% of capillary porosity) were the main soil moisture thresholds affecting the litter-fall. It was suggested that in acid rain region, Masson pine forest was easily to suffer from water deficit stress, especially in dry-summer period. The water deficit stress, together with already existed acid rain stress, would further threaten the health of the Masson forest.
2009年3月至2011年11月,对中国东南部重庆酸雨区马尾松林土壤水分的时空变化及其对针叶凋落的影响进行了调查,并确定了相应的土壤水分阈值。无论年降水量丰富、正常还是低于平均水平,森林土壤水分的季节变化都可明显分为四个时期,即充足期(5月前)、下降期(6 - 7月)、干旱期(8 - 9月)和恢复期(10 - 11月)。随着土壤深度增加,土壤含水量先降低后升高,但不同土层土壤含水量的差异随年降水量减少而减小。森林生长季节月针叶凋落量与根区(0 - 60 cm土层)蓄水量显著相关,尤其是在主根区(20 - 50 cm土层)。土壤田间持水量(或毛管孔隙度)及田间持水量的82%(或毛管孔隙度的80%)是影响凋落物量的主要土壤水分阈值。研究表明,在酸雨区,马尾松林易遭受水分亏缺胁迫,尤其是在夏季干旱期。水分亏缺胁迫与已存在的酸雨胁迫共同作用,将进一步威胁马尾松林的健康。