Effect of Manure Application, Aeration, and Soil pH on Soil Nitrogen Transformations and on Certain Soil Test Values

1970 ◽  
Vol 34 (2) ◽  
pp. 222-225 ◽  
Author(s):  
R. J. Olsen ◽  
R. F. Hensler ◽  
O. J. Attoe
2010 ◽  
Vol 74 (4) ◽  
pp. 1259-1270 ◽  
Author(s):  
Jonathan L. Deenik ◽  
Tai McClellan ◽  
Goro Uehara ◽  
Michael J. Antal ◽  
Sonia Campbell

1975 ◽  
Vol 55 (1) ◽  
pp. 29-34 ◽  
Author(s):  
K. A. MACMILLAN ◽  
T. W. SCOTT ◽  
T. W. BATEMAN

The response of corn (Zea mays L.) to manure that had been treated to minimize odor was investigated in a greenhouse trial with two silt loam soils of pH 4.2 and 7.1. Pretreatment of manure resulted in sources initially high in organic N and NH4+, but low in NO3−. One pretreatment gave high initial NO2− concentrations. In soil at pH 4.2, NH4+ was the major N source utilized by corn grown to 36 days, and dry matter yields were superior to those from soil at pH 7.1 where soluble NO3− was the major source of N. At pH 7.1, NO2− remained in significant quantities and decreased dry matter yields at 6 wk. Soil inorganic N concentrations varied between soils and was attributed to soil pH differences. Rate of NO2− disappearance decreased with increase in soil pH, and NH4+ accumulation increased with decrease in soil pH, whereas NO3+ production was favored by neutral pH conditions. Some NO3− production was observed in pH 4.2 soil after 36 days' incubation


1980 ◽  
Vol 57 (1) ◽  
pp. 31-39 ◽  
Author(s):  
Dolen R. Morris ◽  
Nantakorn Boonkerd ◽  
Yenchai Vasuvat

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