Effects of Asphalt on Some Phases of Soil Structure and Erodibility by Wind

1955 ◽  
Vol 19 (2) ◽  
pp. 125-128 ◽  
Author(s):  
W. S. Chepil
Keyword(s):  
2013 ◽  
Vol 12 (4) ◽  
pp. 741-746 ◽  
Author(s):  
Florian Statescu ◽  
Dorin Cotiusca Zauca ◽  
Lucian Vasile Pavel

1958 ◽  
Vol 22 (5) ◽  
pp. 369 ◽  
Author(s):  
Y. Kawano ◽  
W. E. Holmes
Keyword(s):  

2004 ◽  
Vol 68 (2) ◽  
pp. 346 ◽  
Author(s):  
Keijan Wu ◽  
Naoise Nunan ◽  
John W. Crawford ◽  
Iain M. Young ◽  
Karl Ritz

2017 ◽  
Vol 5 (6) ◽  
pp. 32-39
Author(s):  
ZokpodoKoéssiLié Barnabé ◽  
◽  
AkossouArcadiusYves Justin ◽  
DayouEphrème Dossavi ◽  
DognonFulgence Baudelaire ◽  
...  

1972 ◽  
Vol 52 (3) ◽  
pp. 311-321 ◽  
Author(s):  
K. W. AYRES ◽  
R. G. BUTTON ◽  
E. DE JONG

The relation between soil structure and soil aeration was investigated on undisturbed soil cores from soil horizons exhibiting six distinct kinds of soil structure (prismatic, columnar, blocky, granular, platy, massive) over a broad range of soil texture. Soil aeration was characterized at ⅓ atm suction by measurements of air porosity, relative diffusivity (D/Do) and the rate of oxygen diffusion to a platinum microelectrode (ODR). Aeration was adequate in most of the Chernozemic soil horizons studied; however, aeration in many of the Bnt horizons of the Solonetzic soils was inadequate. Air porosity and D/Do were highly correlated. The regression coefficient for D/Do vs. air porosity for blocky structures was significantly different from that found for the other five structural types. For granular structures a negative correlation was found for ODR vs. air porosity compared with a low positive correlation found for the other structure types.


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