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Distribution Characteristic and Assessment of Soil Organic Matter, Nitrogen and Phosphorus in Soils of New born River Mouth Wetlands

  • Chen, Weifeng (College of Resources and Environment, Shandong Agricultural University, China) ;
  • Ann, Seoung-Won (College of Industrial Science, Kongju National University) ;
  • Shi, Yanxi (College of Resources and Environment, Shandong Agricultural University, China) ;
  • Mi, Qinhua (College of Resources and Environment, Shandong Agricultural University, China)
  • Published : 2003.02.01

Abstract

This paper investigates preliminarily spatial distribution soil organic matter (SOM), nitrogen (N) and phosphorus (P) and its environmental influence in wetland soil of different vegetation landscape in the Yellow River Mouth. The result shows the SOM and total nitrogen (TN), efficient N, efficient P in top layer soils of different vegetation district have significantly different content, The SOM is shown as Calamagrostis epigeios wetlands > Phragmites cmmunis wetlands > Tamarix chinensi wetlands above tidal > Suaeda salsa wetlands in high tidal > Tamarix chinensi wetlands in high tidal > tidal flats, the arrange of the TN and efficient N content is the same except that the content in Suaeda salsa wetlands in high tidal is heavier than Tamarix chinensi wetlands in high tidal. In different vegetation landscape wetland types the vertical change of soil nutrients are obvious except for p, gradually decrease from the upper to the lower. This case reflects the function of the vegetation on the wetland development of soil and proves the wetland soil has the characteristic of new born and bad degree of development. SOM, TN, efficient N and efficient P content in wetland soils have significantly positive correlation, but TP have no correlation with them but efficient p. The contents of TN in wetland soils range from 58~1480 mg/kg, total average content 408 mg/kg, average content of above 30 cm is 625 mg/kg. The range of TP content in the soil is 372~1042 mg/kg, total average is 569 mg/kg, average content of above 20 cm is 611 mg/kg. According the P it occurs mainly as calcium phosphates, and the validity is lower, therefore, N and P in the new born wetlands cannot produce serious impact on the environments at present.

Keywords

References

  1. Yu, X.J., D.L. Ma, 1998, The Ecotone and Agricultural development in the Yellow River Delta, Agro-environmental Protection, 17(2), 91-93.
  2. Xiao, H.L., 1999, Climate change in relation to soil organic matter, Soil and Environment, 8(4), 300-304.
  3. Mitsch, W.J. et al., 1986, Van Nostrand Reinhold Company Inc., Wetlands, New York, 89-125pp.
  4. Bai, J.H., D.W., Y.M. Zhu, et al., 2002, Study on the laws of spatial variation of nitrogen in soil of land in land water ecotones-A case of LWF in Yueliangpao wetland, ACTA Scientiae Circumstantiae, 22(3), 343-348.
  5. Lin, R.G. and J.Y. Wu, 1994, Absorbing and release to phosphate of sedimentary of the Yellow River mouth, ACTA Oceanologica Sinica, 16(4), 82-90.
  6. Song, J.M., 2000, Transferable phosphorus in sediments of the Yellow River Estuary Adjacent Waters, Marin Science, 24(7), 42-45.
  7. Chen, S.Z., J.Z. Zhang,, J. Zhang, 1997, Existing Forms of Phosphorus and its Contention Sediment from River Estuaries and the Laizhou Bay, Coast Project, 16(2), 41-46.
  8. Zhao, Y.M. and C.S. Song, 1995, Scientific Survey of the Yellow River Delta Nature Reserve, China Forestry Publishing House, Beijing.
  9. Fang, H.L., 1999, Wetland Research in the Yellow River Delta with Geographical Information System(GIS) and Environmental Models, Beijing: Institute of Geographic Sciences and Natural Resources Research, CAS.
  10. Wang, Q.B., L.H. Li, X.H. Liu, 1998, Spatial Heterogeneity of Soil Organic Carbon and Total Nitrogen in an Xi Lin River Basin Grassland inner Mongolia, Phytoecologica Sinic, 22(5), 409-414.
  11. Zhang, J.T., 1998, Effects of Global Climate Change on C and N Circulation in Natural Soils, Scientia Geographica sinica, 18(5), 463-471.
  12. Li, Z.P. and X.J. Wang, 2000, Analysis and Evaluation of Soil Organic Matter Dynamics at a Little Region Scale, Scientia Geographica sinica, 20(2), 182-188.
  13. Rong, J.G., J.G. Han, P. Wang, et al., 2001, The Effects of Grazing Intensity on Soil Physics and Chemical Properties, Grassland of China, 23(4), 41-47.
  14. Feng, Q., S.M. Liu, J. Zhang, 2000, Distribution of Phosphorus in Sediment of the Bohai and Yellow Sea, Marin Environmental Science, 20(2), 24-29.
  15. Liu, M., M. Lu, S.Y. Xu, 2000, Phosphorus Species in Aquatic Sediments at the Yangtze Estuary and Shanghai Coast, Earth Science Frontiers, 7, 94-98.
  16. Leivuorim, N., 1992, Sedimentation of trace metals in the Gulf of Bothnia, Chemosphere, 31(8), 3839-3856. https://doi.org/10.1016/0045-6535(95)00257-9
  17. Lin, R.G., 1992, Existence Form of the Inorganic Phosphate in the Sedimentary of the Yellow River Mouth, Oceanologia ET Limnologia Sinica, 23(4), 387-395.