Assessment of Soil Compaction Related to the Bulk Density with Land use Types on Arable Land

• Published in: Korean Journal of Soil Science and Fertilizer Vol. 46; no. 5
• Main Authors: Cho, H.R., RDA, Suwon, Republic of Korea, Jung, K.H., RDA, Suwon, Republic of Korea, Zhang, Y.S., RDA, Suwon, Republic of Korea, Han, K.H., RDA, Suwon, Republic of Korea, Roh, A.S., Gyeonngi-do ARES, Hwaseong, Republic of Korea, Cho, K.R., Gyeonngi-do ARES, Hwaseong, Republic of Korea, Lim, S.J., Gyeonngi-do ARES, Hwaseong, Republic of Korea, Choi, S.C., Gangwon-do ARES, Chuncheon, Republic of korea, Lee, J.I., Chungnam ARES, Yessan, Republic of Korea, Yun, Y.U., Chungnam ARES, Yessan, Republic of Korea, Ahn, B.G., Jeollabuk-do ARES, Iksan, Republic of Korea, Kim, B.H., Jeollanam-do ARES, Naju, Republic of Korea, Park, J.H., Gyeongbuk ARES, Daegu, Republic of Korea, Kim, C.Y., Gyeongbuk ARES, Daegu, Republic of Korea, Park, S.J., Gyeongbuk ARES, Daegu, Republic of Korea
• Format: Journal Article
• Language: Korean
• Published: 01.10.2013
• Subjects: COMPACTACION DEL SUELO; COMPACTAGE DU SOL; Soil bulk density,Land use type,assessment of soil physical properties; SOIL COMPACTION
• ISSN: 0367-6315
• DOI: 10.7745/KJSSF.2013.46.5.333

Soil compaction is affected by soil texture, organic matter (OM), strength (ST) and soil moisture, which is difficult to understand the degree and effects of related factors. The purpose of the study is to assess the impact of them on the compaction with bulk density (BD). The analysis was conducted with data collected from national-wide monitoring sites including 105 upland soils, 246 orchard soils, and 408 paddy soils between 2009 and 2012. The distributions of soil physical properties were measured. The correlation and multi linear regression analysis were performed between soil physical properties using SAS. The regression equation of BD(y) includes ST, gravitational water contents (GWC), and OM as variables commonly, having additional factors, clay content and sand content in paddy soil and upland soil for only subsoil (p0.001). Our results show that the BD could be explained about 40~50% by various physical properties. The regression was mainly determined by ST in orchard and upland soil and by the GWC in paddy soil. To mitigate soil compaction, it is important to maintain the proper level of OM in upland soil and to consider the moisture condition with soil texture in paddy soil when making work plan. Furthermore, it would be recommended the management criteria classified by soil texture for the paddy soils.