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- W2020144833 abstract "Abstract Soil texture had a pronounced effect on ammonia movement and retention. The greatest movement of ammonia occurred in the sand and silt loam soils; and the least movement in the clay. The loss of ammonia from the airdry, acid sandy soil at a 6‐inch depth of application was 44 times the loss from the calcareous clay soil receiving ammonia at comparable moisture and depth. The retentive capacity of a soil for ammonia increased greatly as the texture became heavier. The loss of ammonia from the air‐dry, calcareous clay soil was negligible even at the 3‐inch depth of application. A considerable portion of the nitrogen applied as anhydrous ammonia was lost to the atmosphere or was fixed in some form making it non‐extractable by the chemical analysis used. The amount of ammonia fixed increased with the greater clay content of the soil. The presence of high concentrations of ammonia in a localized area resulted in the partial breakdown of the soil organic matter. As a result of nitrification and the subsequent increase in hydrogen‐ion concentration this condition was no longer observed at the end of 4 weeks of incubation. Ammonia losses were reduced considerably when the application was changed from 40‐inch to 16‐inch spacings and the rate applied per acre was maintained a constant." @default.
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- W2020144833 date "1958-01-01" @default.
- W2020144833 modified "2023-10-01" @default.
- W2020144833 title "The Retention and Reactions of Anhydrous Ammonia on Different Soil Types" @default.
- W2020144833 doi "https://doi.org/10.2136/sssaj1958.03615995002200010012x" @default.
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