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[日本亚热带常绿阔叶林的生态水文特征]

[Eco-hydrological characteristics of a subtropical evergreen broadleaved forest in Japan].

作者信息

Xu Xiaoniu, Wang Qin, Hirata Eiji

机构信息

College of Forestry and Landscape Architecture, Anhui Agricultural University, Hefei, China.

出版信息

Ying Yong Sheng Tai Xue Bao. 2006 Sep;17(9):1570-4.

Abstract

A three years (1998-2000) observation on the eco-hydrological characteristics of Castanopsis sieboldii and Schima wallichii dominated subtropical evergreen broadleaved forest on the Okinawa Island of Japan showed that during the observation period, the mean annual precipitation was 3325 mm, and 42.3% of it was directly or indirectly contributed by typhoon rainfall, implying that typhoon played a very important role in the hydrology of the forest. Through-fall and stem-flow contributed to 53.9% and 30.9% of the annual rainfall, respectively. The higher stem-flow could be due to the high wind velocity, intense rainfall, and the crown morphology of dominant species C. sieboldii with inclined branches and concave-shaped leaves. Interception loss occupied 15.2% of the total rainfall, being the lowest in the range of 15%-30% widely reported for many broadleaved evergreen forests. The annual surface runoff and lateral flow were 1092 mm and 613 mm, respectively, and the high proportion of surface runoff (32.8%) was probably due to the poor physical properties of soil, particularly the low noncapillary porosity (8%-12%), high clay content (51.9%-60.5%), and low infiltration rate (12 ml x min(-1)) in deeper soil layers. The effective and maximum water storage capacity of 0-70 cm soil layer were 85 mm and 324 mm, respectively, and the maximum water-holding capacity of forest floor was 2. 8 mm, which were close to or lower than those of the subtropical and tropical rain forests in China.

摘要

对日本冲绳岛以米槠和木荷为主的亚热带常绿阔叶林生态水文特征进行了为期三年(1998 - 2000年)的观测。结果表明,观测期内年平均降水量为3325毫米,其中42.3%直接或间接来自台风降雨,这意味着台风在该森林水文学中起着非常重要的作用。穿透雨和树干茎流分别占年降雨量的53.9%和30.9%。较高的树干茎流可能归因于高风速、强降雨以及优势种米槠倾斜的树枝和凹形叶片的树冠形态。截留损失占总降雨量的15.2%,在许多常绿阔叶林广泛报道的15% - 30%范围内为最低。年地表径流和侧向径流分别为1092毫米和613毫米,较高比例的地表径流(32.8%)可能是由于土壤物理性质较差,特别是深层土壤中非毛管孔隙度低(8% - 12%)、粘粒含量高(51.9% - 60.5%)以及渗透率低(12毫升×分钟⁻¹)。0 - 70厘米土层的有效和最大持水量分别为85毫米和324毫米,林地最大持水量为2.8毫米,接近或低于中国亚热带和热带雨林的水平。

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