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A Study on Soil Characteristics of Paddy Fields with Re-established Soils
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 Title & Authors
A Study on Soil Characteristics of Paddy Fields with Re-established Soils
Sonn, Yeon-Kyu; Moon, Yong-Hee; Zhang, Yong-Seon; Jung, Kang-Ho; Cho, Hye-Rae; Hyun, Byung-Keun; Shin, Kook-Sik; Han, Kyeong-Hwa;
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 Abstract
Six study sites in Gumi, Goryeong in Gyeongbuk province and Naju in Jeonnam province were selected to investigate soil properties of poorly drained horizons in paddy soils. The horizons were re-established layers which were parent material layers originated from fluvial deposits. Topsoil layers were differentiated from piled parent materials while soil structure of the topsoil layer was massive with striated microstructure. Compaction at soil re-establishment and a lack of structure and aggregate development in these soils may cause the limitation of vertical water movement and result in poorly drained horizons. Soil samples were taken from paddy fields with top soils of sandy loam, silt loam and silty clay loam and re-established soils of coarse and fine texture. The samples were taken from each horizon for the analyses of soil chemical and mineral properties. Soils with re-established soils of coarse texture had greater amounts of sands from top soil texture distributions, while soils with fine texture had greater amounts of silts. Chemical properties of top soils were analyzed from rice cultivated soils at the time of re-establishments and one year after the re-establishments. The coarse texture of the re-established horizons decreased in EC values from 0.23 to , available phosphate values from 112 to , and exchangeable Ca values from 6.6 to . On the other hand, soils with fine texture showed decrease only in pH and exchangeable Ca values. Especially, organic matter and available phosphate contents showed heterogeneous distributions from each horizon. This result may be caused by mixture of plough layer and subsurface layer during and consolidation. Hydraulic conductivity values were low at the boundaries of top soil and parent material layers except SL/coarse soil. Soil microstructure was massive structure without soil clods or pores and showed striated structure. Therefore, re-established paddy fields with fluvial deposits as parent material layers showed limited vertical movements of soil water because of occurrence of compacted layers and less-development of soil clods and aggregates.
 Keywords
Pan;Bt;Micro-morphology;Structure;
 Language
Korean
 Cited by
 References
1.
Berg. R.C. 1984. The origin and earllly genesis of clay bands in youthful sandy soils along Lake Michigan. U.S.A. Geoderma. 32:45-62. crossref(new window)

2.
Beutler, A.N. and J.F. Centurion. 2008. Soil compaction by machine traffic and least limiting water range related to soybean yield. Pesq. agropec. bras., Brasia. 43(11):1591-1600. crossref(new window)

3.
Box, J.E. Jr. 1991. The effect of waterlogging on rooting intermittent flooding on germination and seeding growth of cotton. American Soc. Agri. Eng. 14:567-570.

4.
Buol, S.W. and F.D. Hole. 1959. Some characteristics of clay skins on peds in the B horizon of a Gray-Brown Podzolic soil. Soil Sci. Soc. Am. Proc. 23:239-241. crossref(new window)

5.
Chesworth. W. 1973. The parent material effect and the genesis of soils. Geoderma 10:215-225. crossref(new window)

6.
Dijkerman, J.C., M.G. Cline, and G.W. Olson. 1967. Properties and genesis of textural subsoil lamellae. Soil Sci. 104:7-16. crossref(new window)

7.
Doh, D.H., S.J. Kim, S.K. Jin, and R.C. Jo. 1994. A study on variation of the soil physical characteristics of multiutilized paddy field by the introduction of subsurface drainage facility. Journal of Life Science. 1:87-96.

8.
Gile, L.H. 1979. Holocene soils in eolian sediments of Bailey, County Texas. Soil Sci. Soc. Am. Proc. 43:994-1003. crossref(new window)

9.
Hamza, M.A. and W.K. Anderson. 2003. Responses of soil properties and grain yields to deep ripping and gypsum application in a compacted loamy sand soil contrasted with a sandy clay loam soil in Western Australia. Aust. J. Agric. Res. 54(3):273-282. crossref(new window)

10.
Hamza, M.A. and W.K. Anderson. 2005. Soil compaction in cropping systems. A review of the nature, causes and possible solutions. Soil Tillage Res. 82(2):121-145. crossref(new window)

11.
Han, K.H., I.Y. Kim, S.W. Hwang, H.J. Cho, S.S. Kang, S.O. Hur, D.S. Oh, G.S. Lee, and H.S. Lee. 2009. Research for physical characteristics on soil compaction. NIAST Report. 519-534. (In Korean)

12.
Jeong, G.Y. and S.J. Kim. 1993. Boxwork fabric of halloysite-rich kaolin formed by weathering of anorthite in Sancheong area, Korea. Clays and Clay Minerals, 41:56-65. crossref(new window)

13.
Lee, C.K., Y.K.Sonn, J.H.Sung, I.G. Jung, S.C. Kim, W.P. Park, and W.K. Park. 2002. Geostatistical analysis of spatial variability for field information in paddy field. Kor. J. Intl. Agri. 14(2):127-138.

14.
NIAST. 2000. Soil and plant analysis. (In Korean)

15.
NIAST. 2006. Fertilizer recommendation for crops (revision). National Institute of Agricultural Science and Technology, RDA, Suwon, Korea.

16.
Ponti, D.J. 1985. The quarternary alluvial sequence of the Antelope Valley, Califomia. Geol. Soc. Am. Spec. Pap. 203:79-96.

17.
Reheis, M.C. 1990. Influence of climate and eolian dust on the major-element chemistry and clay mineralogy of soils in the northern Bighom Basin, U.S.A. Catena 17:219-248. crossref(new window)

18.
Stoops, G. and H. Eswaran. 1986. Soil micromorphology. Van Nostrand Rheinhold soil science series. Van Nostrand Reinhold. 345 p.

19.
USDA, NRCS. 2004. Soil survey laboratory methods manual. Soil Survey Investigation Report No. 42. Version 4.0. USDA-NRCS, Washington.

20.
Yun, E.S., K.Y. Jung, K.D. Park, Y.K. Sonn, C.Y. Park, J.B. Hwang, and M.H. Nam. 2011. Compaction characteristics of multi-cropping paddy soils in south-eastern part of Korea. Korean J. Soil Sci. Fert. 44(5):688-695. crossref(new window)

21.
Zhang, Y.S., Y.K. Sonn, S.J. Jung, G.J. Lee, M.S. Kim, S.K. Kim, J.Y. Lee, and I. H. Pyun. 2006. Clay mineral composition of the soils derived from residuum and colluvium. Korean J. Soil Sci. Fert. 39(5): 246-329.