Dynamics of ammonium and pH in the solution of soils with different salinity levels, growing irrigated rice
Rice in Rio Grande do Sul State is grown mostly under flooding, which induces a series of chemical, physical and biological changes in the root environment. These changes, combined with the presence of rice plants, affect the availability of exchangeable ammonium (NH4+) and pH of soil solution, wher...
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| Format: | Article |
| Language: | English |
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Sociedade Brasileira de Ciência do Solo
2012-04-01
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| Series: | Revista Brasileira de Ciência do Solo |
| Subjects: | |
| Online Access: | http://www.scielo.br/scielo.php?script=sci_arttext&pid=S0100-06832012000200009&lng=en&tlng=en |
| _version_ | 1818970941821026304 |
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| author | Felipe de Campos Carmona Ibanor Anghinoni Eduardo Giacomelli Cao |
| author_facet | Felipe de Campos Carmona Ibanor Anghinoni Eduardo Giacomelli Cao |
| author_sort | Felipe de Campos Carmona |
| collection | DOAJ |
| description | Rice in Rio Grande do Sul State is grown mostly under flooding, which induces a series of chemical, physical and biological changes in the root environment. These changes, combined with the presence of rice plants, affect the availability of exchangeable ammonium (NH4+) and pH of soil solution, whereas the dynamics of both variables can be influenced by soil salinity, a common problem in the coastal region. This study was conducted to evaluate the dynamics of exchangeable NH4+ and pH in the soil solution, and their relation in the solution of Albaqualf soils with different salinity levels, under rice. Four field experiments were conducted with soils with exchangeable Na percentage (ESP) of 5.6, 9.0, 21.2, and 32.7 %. Prior to flooding, soil solution collectors were installed at depths of 5, 10 and 20 cm. The soil solution was collected weekly, from 7 to 91 days after flooding (DAF), to analyze exchangeable NH4+ and pH in the samples. Plant tissue was sampled 77 DAF, to determine N uptake and estimate the contribution of other N forms to rice nutrition. The content of exchangeable NH4+ decreased over time at all sites and depths, with a more pronounced reduction in soils with lower salinity levels, reaching values close to zero. A possible contribution of non-exchangeable NH4+ forms and N from soil organic matter to rice nutrition was observed. Soil pH decreased with time in soils with ESP 5.6 and 9.0 %, being positively correlated with the decreasing NH4+ levels at these sites. |
| first_indexed | 2024-12-20T14:44:29Z |
| format | Article |
| id | doaj.art-5de955429843490aa793dc87d0fad7e3 |
| institution | Directory Open Access Journal |
| issn | 1806-9657 |
| language | English |
| last_indexed | 2024-12-20T14:44:29Z |
| publishDate | 2012-04-01 |
| publisher | Sociedade Brasileira de Ciência do Solo |
| record_format | Article |
| series | Revista Brasileira de Ciência do Solo |
| spelling | doaj.art-5de955429843490aa793dc87d0fad7e32022-12-21T19:37:10ZengSociedade Brasileira de Ciência do SoloRevista Brasileira de Ciência do Solo1806-96572012-04-0136240140910.1590/S0100-06832012000200009S0100-06832012000200009Dynamics of ammonium and pH in the solution of soils with different salinity levels, growing irrigated riceFelipe de Campos CarmonaIbanor Anghinoni0Eduardo Giacomelli CaoUniversidade Federal do Rio Grande do SulRice in Rio Grande do Sul State is grown mostly under flooding, which induces a series of chemical, physical and biological changes in the root environment. These changes, combined with the presence of rice plants, affect the availability of exchangeable ammonium (NH4+) and pH of soil solution, whereas the dynamics of both variables can be influenced by soil salinity, a common problem in the coastal region. This study was conducted to evaluate the dynamics of exchangeable NH4+ and pH in the soil solution, and their relation in the solution of Albaqualf soils with different salinity levels, under rice. Four field experiments were conducted with soils with exchangeable Na percentage (ESP) of 5.6, 9.0, 21.2, and 32.7 %. Prior to flooding, soil solution collectors were installed at depths of 5, 10 and 20 cm. The soil solution was collected weekly, from 7 to 91 days after flooding (DAF), to analyze exchangeable NH4+ and pH in the samples. Plant tissue was sampled 77 DAF, to determine N uptake and estimate the contribution of other N forms to rice nutrition. The content of exchangeable NH4+ decreased over time at all sites and depths, with a more pronounced reduction in soils with lower salinity levels, reaching values close to zero. A possible contribution of non-exchangeable NH4+ forms and N from soil organic matter to rice nutrition was observed. Soil pH decreased with time in soils with ESP 5.6 and 9.0 %, being positively correlated with the decreasing NH4+ levels at these sites.http://www.scielo.br/scielo.php?script=sci_arttext&pid=S0100-06832012000200009&lng=en&tlng=ennitrogênioacidezpercentagem de sódio trocável |
| spellingShingle | Felipe de Campos Carmona Ibanor Anghinoni Eduardo Giacomelli Cao Dynamics of ammonium and pH in the solution of soils with different salinity levels, growing irrigated rice Revista Brasileira de Ciência do Solo nitrogênio acidez percentagem de sódio trocável |
| title | Dynamics of ammonium and pH in the solution of soils with different salinity levels, growing irrigated rice |
| title_full | Dynamics of ammonium and pH in the solution of soils with different salinity levels, growing irrigated rice |
| title_fullStr | Dynamics of ammonium and pH in the solution of soils with different salinity levels, growing irrigated rice |
| title_full_unstemmed | Dynamics of ammonium and pH in the solution of soils with different salinity levels, growing irrigated rice |
| title_short | Dynamics of ammonium and pH in the solution of soils with different salinity levels, growing irrigated rice |
| title_sort | dynamics of ammonium and ph in the solution of soils with different salinity levels growing irrigated rice |
| topic | nitrogênio acidez percentagem de sódio trocável |
| url | http://www.scielo.br/scielo.php?script=sci_arttext&pid=S0100-06832012000200009&lng=en&tlng=en |
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