2007
DOI: 10.1016/j.biosystemseng.2007.03.006
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Suitability of pre-compression stress as the real critical stress of unsaturated agricultural soils

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Cited by 32 publications
(18 citation statements)
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“…Finally, we can also define the effect of the recovery process on the preferred orientation of soil pores as it depends on the pore distribution before loading, the magnitude of the applied stresses and their direction (Cetin 2004). Higher air conductivity values prior the test at LCh UG79 compared with SG UG79 can be explained with more connected pores of a given diameter (Mosaddeghi et al 2007) at the LCh site which indicates better soil recovery from grazing at this site. This is also in agreement with our previous findings.…”
Section: Discussionmentioning
confidence: 98%
“…Finally, we can also define the effect of the recovery process on the preferred orientation of soil pores as it depends on the pore distribution before loading, the magnitude of the applied stresses and their direction (Cetin 2004). Higher air conductivity values prior the test at LCh UG79 compared with SG UG79 can be explained with more connected pores of a given diameter (Mosaddeghi et al 2007) at the LCh site which indicates better soil recovery from grazing at this site. This is also in agreement with our previous findings.…”
Section: Discussionmentioning
confidence: 98%
“…One of the drawbacks, however, is that larger machinery usually means increased machinery weight, which increases the risk of soil damage due to compaction (Raper, 2005). This issue has brought about increased questioning on the maximum acceptable mechanical compressibility of arable soils (Mosaddeghi et al, 2007).…”
mentioning
confidence: 99%
“…Esta redução ocorre devido à expulsão do ar e da água, e preenchimento de parte dos vazios pela fase sólida (Schäffer et al, 2007). Como a aplicação da pressão é feita em um intervalo de tempo muito curto, a redução na porosidade se deve à diminuição do volume de macroporos e expulsão da fase gasosa (Mosaddeghi et al, 2007) e disto decorre uma perda de porosidade também em intervalo de tempo extremamente curto, o que coloca, com instantaneidade, o solo recuperado novamente em condições físicas semelhantes ao degradado.…”
Section: Bunclassified
“…As relações pressão-deformação são complexas e diferem muito entre solos e, no mesmo solo, variam com o conteúdo de água (Gregory et al, 2006). Segundo Mosaddeghi et al (2007), a mudança de volume pode ser expressa pelo índice de vazios (razão entre o volume de vazios ou poros e o volume de partícu-las), porosidade ou densidade do solo. Essas relações dependem de características do solo e da história de tensões por ele sofridas sendo expressas, genericamente, pela curva de compressão do solo .…”
Section: Introductionunclassified