ISSN : 2287-8327
In order to elucidate the mechanisms affecting plant distributions in the reclaimed dredging area in the Gwangyang steelworks, in the Gwangyang Bay, Korea, we examined soil characteristics and plant distributions in four study sites and a control site in the study area. Desalination occurring along a gradient with increasing elevation, resulting in decrease of soil pH, EC, P, K, Cl, Ca, Mg, and salt and an increase in soil T-N, silt, clay contents. From site 1 (the lowest-elevation site) to site 5 (the highest-elevation site), halophytes decreased in abundance and nonhalophytes increased. The dominant species in each site were: Phragmites communis, Limonium tetragonum, and 12 additional species at site 1, Carex pumila, Suaeda japonica, and 15 additional species at site 2, Spergularia marina, Scirpus planiculmis, and 22 additional species at site 3, Miscantus sinensis, Lespedeza bicolor, and 26 additional species at site 4 and Pinus thunberii, Rhododendron mucronulatum, and 39 additional species at site 5, which resembled a naturally-occurring P. thinbergii community. Cluster analysis of the vegetation data matrix grouped the 35 plots into 5 major groups, and cluster analysis using the soil environment data matrix revealed 4 major groups. CCA of the floristic and environmental data matrix showed a positive relationship of SAR, EC, Na, Cl, and Ca, which are related to salt, in the 1st axis and 2nd axis, but negative relationships for altitude, organic contents, silt, and clay contents. Notably, plant species in the reclaimed dredging area that were separated along the 1st axis showed strong relationships with factors that related to salt. Long-term exposure to natural rainfall in the reclaimed dredging area changed the soil characteristics, such as salinity. This change in soil characteristics might alter the SAR, which affects plant survival strategies in a given habitat. These results strongly indicated that factors related to salt and elevation play important roles in determining the overall plant distribution in the reclaimed dredging area.
Ajimal KM, Aziz S. 1998. Some aspects of salinity, plant density and nutrient effects on Cressa cretica L. J Plant Nut 21: 769-784.
Allen SE, Grimshaw HM, Rowland AP. 1986. Chemical analysis. In Method in Plant Ecology (Moore PD, Chapman SB, eds). Blackwell Sci Publ, Oxford, pp 285-344.
Barbour HG. 1970. Is any angiosperm an obligate halophyte? Am Mid Nat 84: 106-119.
Bertness MD, Gough L, Shumway SW. 1992. Salt tolerance and distribution of fugitive salt marsh plants. Ecology 73: 1842-1851.
Bouma T, Bas J, Koutstaal P, Van Dongen M, Nielsen KL. 2001. Coping with low nutrient availability and inundation: root growth responses of three halophytic grass species from different elevations along a flooding gradient. Oecologia 126: 474-481.
Chapman VJ. 1977. Wet coastal ecosystems; ecosystems of the world. BUMBA Vol (1), Amsterdam.
Christopher C, Broome S, Campbell C. 2002. Fifteen years of vegetation and soil development after brackish-water marsh creation. Rest Ecol 10: 248-258.
Choung YS, Kim JH. 1991. Studies on the population biology of some clonal plants in a coastal reclaimed land. I. Rhizome architecture, patch formation and growth of Calamagrostis epigeios plants. Korean J Ecol 14: 327-343.
Connell JH, Slatyer RO. 1977. Mechanisms of succession in natural communities and their role in community stability and organization. Am Nat 111: 1119-1144.
Greenway H, Munns R. 1980. Mechanisms of salt tolerance in nonhalophytes. Ann Rev Plant Physiol 31: 149-190.
Hong SW, Hah YC, Choi YK. 1970. Ecological studies of the certain halophyte on the high saline soil. Korean J Bot 13: 25-32.
Kwak YS, Hur YK, Song JH, Hwangbo JK. 2004. Quantification of atmospheric purification capacity by forestation impact assessment of Gwangyang steel works. J RIST 18: 334-340.
Lee SK, Goh KC, Yee SO. 1996. Natural regeneration of vegetation as an alternative for greening sand filled reclaimed land in Singapore. Land Degrad Develop 8: 59-70.
Min BM. 1985. Changes of soil and vegetation in coastal reclaimed lands, west coast of Korea. Ph.D. Thesis. Seoul Natl Univ, Seoul.
Min BM, Kim JH. 1999a. Plant community structure in reclaimed land on the west coast of Korea. J Plant Biol 42: 287-293.
Min BM, Kim JH. 1999b. Plant distribution in relation to soil properties of reclaimed lands on the west coast of Korea. J Plant Biol 42: 279-286.
Min BM, Kim JH, Kimura M, Kikuchi E, Suzuki K, Takeda S, Kurihara Y. 1989. Soil and plant community of reclaimed lands on the west coast of Korea. Ecol Rev 21: 245-257.
Muller-Dombois D, Ellenberg H. 1974, Aims and Methods of Vegetation Ecology. Wiley international edition, New York.
Nam W, Kwak YS, Jeong IH, Lee DB, Lee SS. 2008a. Plant distributions and physicochemical characteristics of topsoil on the reclaimed dredging area. J Korean Inst Landscape Architec 36: 52-62.
Nam W, Kwak YS, Jeong IH, Lee DB, Lee SS. 2008b. Physicochemical properties of depth-based soil on the reclaimed dredging area. J Korean Env Reveg Tech 11: 60-71.
Orloci L. 1978. Multi-variate Analysis in Vegetation Research. 2nd Ed. W- Junk, The Hague.
Pennings SC, Callaway RM. 1992. Salt marsh plant zonation: the relative importance of competition and physical factors. Ecology 73: 681-690.
Richard C, Chmura GL. 2000. Dynamic of above- and belowground organic matter in a high latitude macrotidal saltmarsh. Marine Ecol 204: 101-110.
Sally T, Zedler, JB. 2000. Site conditions, not parental phenotype, determine the height of Spartina foliosa. Estuaries 23: 572-582.
Seliskar DM, Gallagher JL, Burdick DM, Mutz LA. 2002. The regulation of ecosystem function by ecotypic variation in the dominant plant: a Spartina alterniflora salt marsh case study. J Ecol 90: 1-11.
Silvestri S, Andrea D, Marco M. 2005. Tidal regime, salinity and salt marsh plant zonation. Estuar Coast Shelf Sci 62: 119-130.