ISSN:
1432-0789
Keywords:
Interlayer ammonium
;
Beet
;
Clay minerals
;
K concentration
;
Nitrogen turnover
Source:
Springer Online Journal Archives 1860-2000
Topics:
Biology
,
Geosciences
,
Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
Notes:
Abstract We studied the turnover of interlayer NH inf4 sup+ in three soils cropped with sugar beet. The three soils chosen for this study (Carpi, Cadriano, and Ozzano) are typical of the soils in the Po Valley where sugar beet is grown. The variation in interlayer NH inf4 sup+ content during the growing season was significant and very similar for the Carpi and Cadriano soils, while there was no significant variation in the NH inf4 sup+ content in the Ozzano soil during the same period. The turnover of interlayer NH inf4 sup+ in the Carpi and Cadriano soils was high, and appeared to cover a substantial amount of the N requirement of the crop. The turnover in these two soils showed a significant decrease during the initial phase followed by a period during which the pool of interlayer NH inf4 sup+ was replenished and reached the initial levels again. The spatial distribution of the root system, the pattern of N uptake by the sugar beet crop, and the processes of immobilization-mineralization of organic N all have an influence on the mechanisms of adsorption and release of interlayer NH inf4 sup+ . The release of interlayer NH inf4 sup+ , and thus its availability for plant uptake, was greater at the beginning of the growing season. The physicochemical characteristics of the soils, the K concentration, and the types of clay minerals present were found to be important in determining the dynamics of interlayer NH inf4 sup+ turnover of soils.
Type of Medium:
Electronic Resource
URL:
http://dx.doi.org/10.1007/BF00336440
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