FATE OF ADDED NITROGEN IN SOILS

The transformation of added N in some Manitoba soils was studied in the laboratory. Addition of urea-N to acid soils led to accumulation of nitrite ions and some of this nitrogen was chemically dent-rifled. The initial rate of molecular N production was 3.2% of added N02 per day in acid Well wood so...

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Główni autorzy: OLU-OBI, A., HEDLIN , R. A., CHO, C. M.
Format: Online
Język:angielski
Wydane: The Faculty of Agriculture Obafemi Awolowo University, Ile-Ife, Nigeria. 2020
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Dostęp online:https://ija.oauife.edu.ng/index.php/ija/article/view/577
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author OLU-OBI, A.
HEDLIN , R. A.
CHO, C. M.
author_facet OLU-OBI, A.
HEDLIN , R. A.
CHO, C. M.
author_sort OLU-OBI, A.
collection OJS
description The transformation of added N in some Manitoba soils was studied in the laboratory. Addition of urea-N to acid soils led to accumulation of nitrite ions and some of this nitrogen was chemically dent-rifled. The initial rate of molecular N production was 3.2% of added N02 per day in acid Well wood soil and 1.4% for acid Pine Ridge soil. Nitrite ions also accumulated in the calcareous Almasippi soil (pH 7.7) for a short period, but was denitrified. Oxidation of ammonium ions was very slow in the acid soil. Soil fixation of added N was greater at low than at high soil pH, and soil organic matter fixed approximately 5 to 10 times as much N per unit weight as did clay. Liming the acid soils considerably reduced the amount of added N fixed.
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spelling oai:ojs2.ija.oauife.edu.ng:article-5772020-10-08T09:13:37Z FATE OF ADDED NITROGEN IN SOILS OLU-OBI, A. HEDLIN , R. A. CHO, C. M. Urea-N, nitrite ions, acid soils, soil fixation, liming, calcareous The transformation of added N in some Manitoba soils was studied in the laboratory. Addition of urea-N to acid soils led to accumulation of nitrite ions and some of this nitrogen was chemically dent-rifled. The initial rate of molecular N production was 3.2% of added N02 per day in acid Well wood soil and 1.4% for acid Pine Ridge soil. Nitrite ions also accumulated in the calcareous Almasippi soil (pH 7.7) for a short period, but was denitrified. Oxidation of ammonium ions was very slow in the acid soil. Soil fixation of added N was greater at low than at high soil pH, and soil organic matter fixed approximately 5 to 10 times as much N per unit weight as did clay. Liming the acid soils considerably reduced the amount of added N fixed. The Faculty of Agriculture Obafemi Awolowo University, Ile-Ife, Nigeria. 2020-10-08 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion Peer-reviewed Article application/pdf https://ija.oauife.edu.ng/index.php/ija/article/view/577 Ife Journal of Agriculture; Vol. 17 No. 1 (1995): Ife Journal of Agriculture; 142-150 0331-6351 eng https://ija.oauife.edu.ng/index.php/ija/article/view/577/462 Copyright (c) 2020 Ife Journal of Agriculture
spellingShingle Urea-N, nitrite ions, acid soils, soil fixation, liming, calcareous
OLU-OBI, A.
HEDLIN , R. A.
CHO, C. M.
FATE OF ADDED NITROGEN IN SOILS
title FATE OF ADDED NITROGEN IN SOILS
title_full FATE OF ADDED NITROGEN IN SOILS
title_fullStr FATE OF ADDED NITROGEN IN SOILS
title_full_unstemmed FATE OF ADDED NITROGEN IN SOILS
title_short FATE OF ADDED NITROGEN IN SOILS
title_sort fate of added nitrogen in soils
topic Urea-N, nitrite ions, acid soils, soil fixation, liming, calcareous
topic_facet Urea-N, nitrite ions, acid soils, soil fixation, liming, calcareous
url https://ija.oauife.edu.ng/index.php/ija/article/view/577
work_keys_str_mv AT oluobia fateofaddednitrogeninsoils
AT hedlinra fateofaddednitrogeninsoils
AT chocm fateofaddednitrogeninsoils