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Effects of soil burial depth on the seed germination of Phragmites australis and Typha domingensis.

MENG Huan1,2, WANG Xue-hong1, TONG Shou-zheng1**, LU Xian-guo1, ZHANG Wen-guang1, HUO Li-li1,2, LOU Xiao-nan1, MENG Xian-kun3   

  1. (1Research Center for Wetland Ecology and Environment, Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, Changchun 130012, China; 2University of Chinese Academy of Sciences, Beijing 100049, China; 3Nature Reserve Administration of Wetland along the Songhua River in Fujin, Fujin 156100, Heilongjiang, China)
  • Online:2013-09-10 Published:2013-09-10

Abstract: Soil burial depth is one of the key factors affecting the seed germination and seedling growth of wetland plants. In this paper, a laboratory simulation experiment was conducted to study the effects of soil burial depths (0, 5, 10, 15, 20, 25, and 30 mm) on the seed germination percentage (GP), germination speed (GS), shoot length (SL), and root length (RL) of Phragmites australis and Typha domingensis in the riparian wetlands along the downstream of Songhua River, Northeast China. The main objective of this study was to provide the technique and strategy for guiding vegetation restoration via sexual reproduction approaches for P. australis and T. domingensis along the downstream of Songhua River. Significant effects of soil burial depth on the GP and GS were observed for both P. australis and T. domingensis. The seed GP and GS of P. australis and T. domingensis varied with soil burial depth. The seed GP and GS of P. australis were higher when the soil burial depths 0 mm and 25 mm, while those of T. domingensis were higher when the soil burial depths were 0 mm and > 25 mm. From the viewpoints of SL and RL, the soil burial depths of < 10 mm were more beneficial to the survival and growth of P. australis and T. domingensis. At the same soil burial depths, the seeds of P. australis had stronger germination ability than those of T. domingensis.

Key words: meteorological parameters., evapotranspiration, eddy covariance method, Penman-Monteith model