Temperature during soybean seed storage and the amount of electrolytes of soaked seeds solution

The electrical conductivity test measures the electrolytes that leach out of seeds when they are immersed in water and this leakage is an indication of seed vigor. The level of standardization reached by the procedures of this test is such that the test is recommended for pea seeds and suggested for other large seeded legumes, including soybean [Glycine max (L.) Merrill]. This study was conducted to contribute to the standardization of this test for soybean seeds by verifying whether the seed storage temperature influences the composition of the leachate from soaked seeds solution. Two soybean seed lots of distinct physiological potential were stored in moisture-proof containers either at constant temperatures of 10ºC and 20ºC or at the temperature of 20ºC during the first seven months of storage followed by a change to 10ºC for the rest of the storage time (nine months). The chemical composition of the soaked water was evaluated every three months from January to October 1998. The highest amount of leakage was observed for potassium, followed by calcium and magnesium, iron and sodium regardless of temperature and storage period. The amount of electrolytes in the soaked water increased as the period of time and the temperature of storage increased. On the other hand the amount of leakage decrease along the time for those seeds stored at 10ºC or transferred from the temperature of 20 to that of 10ºC. The temperature at which soybean seeds remain during storage may affect the amount of electrolytes in the soaked water and consequently the results of the electrical conductivity test.O teste de condutividade elétrica mede a quantidade de eletrólitos liberada das sementes quando imersas em água, sendo um indicador do vigor da semente. O teste é recomendado para sementes de ervilha e sugerido para outras leguminosas, incluindo a soja [Glycine max (L.) Merrill]. O presente trabalho visa contribuir para a padronização do referido teste para avaliação do vigor de sementes de soja, procurando verificar se a temperatura de armazenamento da semente pode influenciar a liberação de eletrólitos na solução de embebição das sementes. Dois lotes de sementes de soja de potenciais fisiológicos distintos foram acondicionados em embalagens herméticas e armazenados em três ambientes: 10 e 20ºC (constantes) e 20ºC por sete meses, com transferência para 10ºC até o final do armazenamento (mais nove meses). A composição química da solução de embebição das sementes foi analisada a cada período de três meses, de janeiro a outubro de 1998. Os maiores valores de lixiviação foram observados para potássio, seguido de cálcio e magnésio, ferro e sódio. Verificou-se acréscimo na quantidade de eletrólitos na solução de embebição em função do aumento do período e da temperatura de armazenamento. Por outro lado, observou-se decréscimo na quantidade de lixiviados ao longo do tempo para as sementes armazenadas a 10ºC ou transferidas da temperatura de 20ºC para 10ºC. A temperatura de armazenamento de sementes de soja pode interferir na liberação de eletrólitos na solução de embebição e, conseqüentemente, nos resultados do teste de condutividade elétrica

Photosynthetic Rate of Three Soybean (Glycine Max (L.) Merrill) Communities as Related to Carbon-Dioxide Levels and Solar Radiation

85 p.Thesis (Ph.D.)--University of Illinois at Urbana-Champaign, 1969.U of I OnlyRestricted to the U of I community indefinitely during batch ingest of legacy ETD

Magnetic properties of marine magnetotactic bacteria in a seasonally stratified coastal pond (Salt Pond, MA, USA)

Magnetic properties of suspended material in the water columns of freshwater and marine environments provide snapshots of magnetic biomineralization that have yet to be affected by the eventual time-integration and early diagenetic effects that occur after sediment deposition. Here, we report on the magnetism, geochemistry and geobiology of uncultured magnetite- and greigite-producing magnetotactic bacteria (MB) and magnetically responsive protists (MRP) in Salt Pond (Falmouth, MA, USA), a small coastal, marine basin (∼5 m deep) that becomes chemically stratified during the summer months. At this time, strong inverse O2 and H2S concentration gradients form in the water column and a well-defined oxic–anoxic interface (OAI) is established at a water depth of about 3.5 m. At least four morphological types of MB, both magnetite and greigite producers, and several species of magnetically responsive protists are found associated with the OAI and the lower sulphidic hypolimnion. Magnetic properties of filtered water were determined through the water column across the OAI and were consistent with the occurrence of magnetite- and greigite-producing MB at different depths. Sharp peaks in anhysteretic remanent magnetization (ARM) and saturation isothermal remanent magnetization (SIRM) and single-domain (SD) values of ARM/SIRM occur within the OAI corresponding to high concentrations of MB and MRP with magnetically derived cell densities of 104–106 ml−1. Low-temperature (K) remanence indicated that while only magnetite producers inhabit the OAI, both magnetite and greigite producers inhabit the sulphidic hypolimnion below the OAI. Magnetic measurements also show that the amount of Fe sequestered in magnetite magnetosomes within the OAI is no more than 3.3 per cent of the total available dissolved Fe(II) in the water column. However, below the OAI, magnetic minerals constitute a much larger fraction of the total dissolved Fe(II) ranging from 13.6 to 32.2 per cent depending on magnetic mineralogy. Most of this iron is possibly in the form of nanophase magnetic particles, possibly associated with biologically induced mineralization processes occurring below the OAI. Still, the OAI is a narrow but intense zone of SD particle production. Despite using just a small fraction of available dissolved Fe(II) in the water column for magnetosome production, the total number of MB living within an OAI, such as at Salt Pond, is all that is needed to produce the biogenic SD concentrations observed in some sediments. We also observed that Verwey transition temperatures fell within a narrow range of values between 95 and 105 K that were independent of both water depth and geochemical conditions. Reduced Verwey transition temperatures (Tv \u3c 120 K) appear to be an intrinsic property of magnetite magnetosomes whether grown in pure laboratory cultures or from a diverse population of magnetite-producing MB in the environment. This indicates that a limited amount of oxygen non-stoichiometry

Tempertatura de armazenamento e quantidade de lixiviados na solução de embeição de sementes de soja

O teste de condutividade elétrica mede a quantidade de eletrólitos liberada das sementes quando imersas em água, sendo um indicador do vigor da semente. O teste é recomendado para sementes de ervilha e sugerido para outras leguminosas, incluindo a soja [Glycine max (L.) Merrill]. O presente trabalho visa contribuir para a padronização do referido teste para avaliação do vigor de sementes de soja, procurando verificar se a temperatura de armazenamento da semente pode influenciar a liberação de eletrólitos na solução de embebição das sementes. Dois lotes de sementes de soja de potenciais fisiológicos distintos foram acondicionados em embalagens herméticas e armazenados em três ambientes: 10 e 20ºC (constantes) e 20ºC por sete meses, com transferência para 10ºC até o final do armazenamento (mais nove meses). A composição química da solução de embebição das sementes foi analisada a cada período de três meses, de janeiro a outubro de 1998. Os maiores valores de lixiviação foram observados para potássio, seguido de cálcio e magnésio, ferro e sódio. Verificou-se acréscimo na quantidade de eletrólitos na solução de embebição em função do aumento do período e da temperatura de armazenamento. Por outro lado, observou-se decréscimo na quantidade de lixiviados ao longo do tempo para as sementes armazenadas a 10ºC ou transferidas da temperatura de 20ºC para 10ºC. A temperatura de armazenamento de sementes de soja pode interferir na liberação de eletrólitos na solução de embebição e, conseqüentemente, nos resultados do teste de condutividade elétrica.The electrical conductivity test measures the electrolytes that leach out of seeds when they are immersed in water and this leakage is an indication of seed vigor. The level of standardization reached by the procedures of this test is such that the test is recommended for pea seeds and suggested for other large seeded legumes, including soybean [Glycine max (L.) Merrill]. This study was conducted to contribute to the standardization of this test for soybean seeds by verifying whether the seed storage temperature influences the composition of the leachate from soaked seeds solution. Two soybean seed lots of distinct physiological potential were stored in moisture-proof containers either at constant temperatures of 10ºC and 20ºC or at the temperature of 20ºC during the first seven months of storage followed by a change to 10ºC for the rest of the storage time (nine months). The chemical composition of the soaked water was evaluated every three months from January to October 1998. The highest amount of leakage was observed for potassium, followed by calcium and magnesium, iron and sodium regardless of temperature and storage period. The amount of electrolytes in the soaked water increased as the period of time and the temperature of storage increased. on the other hand the amount of leakage decrease along the time for those seeds stored at 10ºC or transferred from the temperature of 20 to that of 10ºC. The temperature at which soybean seeds remain during storage may affect the amount of electrolytes in the soaked water and consequently the results of the electrical conductivity test