On seasonal fluctuations of available Olsen P in soils

The likelihood of a strong seasonal effect on the analytical results of soil chemical tests has been substantiated by several findings. The occurrence of such a trouble would heavily affect the routine work of chemical laboratories dealing with hundreds or thousands of soil samples every year and wo...

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Main Authors: Vincenzo Tabaglio, Carolina Gavazzi, Paolo Paris
Format: Article
Language:English
Published: PAGEPress Publications 2006-03-01
Series:Italian Journal of Agronomy
Subjects:
Online Access:https://www.agronomy.it/index.php/agro/article/view/33
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spelling doaj-0552f3f2986a475897eec9638cbbbf092020-11-24T23:30:57ZengPAGEPress PublicationsItalian Journal of Agronomy1125-47182039-68052006-03-011110.4081/ija.2006.73On seasonal fluctuations of available Olsen P in soilsVincenzo TabaglioCarolina GavazziPaolo ParisThe likelihood of a strong seasonal effect on the analytical results of soil chemical tests has been substantiated by several findings. The occurrence of such a trouble would heavily affect the routine work of chemical laboratories dealing with hundreds or thousands of soil samples every year and would possibly interfere even with current timing of soil sampling and testing in agronomical research. Soils from four different experimental fields were sampled and analyzed for Olsen P test through the growing season of both spring-summer crops (maize) and autumn-spring crops (soft wheat). To avoid the cross effect of recent P applications, samples were collected only from the control plots, with no P applied. In a first long-time experiment the level of Olsen P was followed in three soils during two years, while in a second experiment the study considered two different soils for a couple of years each. The amount of extractable (available) Olsen P showed significant fluctuations-with-time in four years out of six. The observed variations seems entirely due to P absorption by crops, as they appeared in the final samplings during the cropping season. The amount of decrease was nearly always small, less than 1-1.5 mg kg-1 soil, and consistent with the reduction of the available pool which is to be expected as crops gradually take up nutrients. As far as Olsen P is concerned, no evidence was found for the occurrence of erratic seasonal variations such as those previously reported. As soil samples for advisory purposes are usually taken at different times of the year, it seems reassuring that no complications are to be expected about information needed to interpret the results of chemical tests.https://www.agronomy.it/index.php/agro/article/view/33Olsen Pchemical testseasonal fluctuation
collection DOAJ
language English
format Article
sources DOAJ
author Vincenzo Tabaglio
Carolina Gavazzi
Paolo Paris
spellingShingle Vincenzo Tabaglio
Carolina Gavazzi
Paolo Paris
On seasonal fluctuations of available Olsen P in soils
Italian Journal of Agronomy
Olsen P
chemical test
seasonal fluctuation
author_facet Vincenzo Tabaglio
Carolina Gavazzi
Paolo Paris
author_sort Vincenzo Tabaglio
title On seasonal fluctuations of available Olsen P in soils
title_short On seasonal fluctuations of available Olsen P in soils
title_full On seasonal fluctuations of available Olsen P in soils
title_fullStr On seasonal fluctuations of available Olsen P in soils
title_full_unstemmed On seasonal fluctuations of available Olsen P in soils
title_sort on seasonal fluctuations of available olsen p in soils
publisher PAGEPress Publications
series Italian Journal of Agronomy
issn 1125-4718
2039-6805
publishDate 2006-03-01
description The likelihood of a strong seasonal effect on the analytical results of soil chemical tests has been substantiated by several findings. The occurrence of such a trouble would heavily affect the routine work of chemical laboratories dealing with hundreds or thousands of soil samples every year and would possibly interfere even with current timing of soil sampling and testing in agronomical research. Soils from four different experimental fields were sampled and analyzed for Olsen P test through the growing season of both spring-summer crops (maize) and autumn-spring crops (soft wheat). To avoid the cross effect of recent P applications, samples were collected only from the control plots, with no P applied. In a first long-time experiment the level of Olsen P was followed in three soils during two years, while in a second experiment the study considered two different soils for a couple of years each. The amount of extractable (available) Olsen P showed significant fluctuations-with-time in four years out of six. The observed variations seems entirely due to P absorption by crops, as they appeared in the final samplings during the cropping season. The amount of decrease was nearly always small, less than 1-1.5 mg kg-1 soil, and consistent with the reduction of the available pool which is to be expected as crops gradually take up nutrients. As far as Olsen P is concerned, no evidence was found for the occurrence of erratic seasonal variations such as those previously reported. As soil samples for advisory purposes are usually taken at different times of the year, it seems reassuring that no complications are to be expected about information needed to interpret the results of chemical tests.
topic Olsen P
chemical test
seasonal fluctuation
url https://www.agronomy.it/index.php/agro/article/view/33
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