R. Lăcătuşu, Mihaela Monica Stanciu-Burileanu, I. Rîşnoveanu, M. Lungu, N. Rizea, A. Lăcătușu, R. Lazăr
{"title":"SELENIUM IN SALSODISOLS LOCATED IN THE CĂLMĂŢUI AND BUZĂU RIVERS VALLEYS","authors":"R. Lăcătuşu, Mihaela Monica Stanciu-Burileanu, I. Rîşnoveanu, M. Lungu, N. Rizea, A. Lăcătușu, R. Lazăr","doi":"10.15551/FPPZT.V11I1.466","DOIUrl":null,"url":null,"abstract":"Selenium contents were determined in the A horizon of the Salsodisols (Solonchaks and Solonetz) placed along the Călmăţui and Buzău Valleys. The total selenium content oscillated between 480 and 1140 g·kg -1 , with an average value of 800 g·kg -1 . This value is 2.1 times higher than the selenium total content in the upper horizon of the World’s non-halomorphic soils. It is also higher than the selenium total content in the upper horizon of the soils from Dobrogea and the South-Eastern Romanian Plain, 5.6 respectively 3.4 times. The mobile selenium content, soluble in the EDTA-CH3COONH4 solution at pH = 7, ranged in the 13-25 g·kg -1 interval, with an average value of 18 g·kg -1 , 4 times higher than the mobile selenium contents of the Dobrogea soils upper horizon and 1.2 times higher than the ones in the South-Eastern part of the Romanian Plain. Between the selenium total contents and some Salsodisols physical and chemical properties proportionality relations were established, statistically ensured. Most of these soils’ selenium content is to be found as calcium, sodium, or magnesium (secondary) selenates. The presence of the same cations’ selenites is not excluded. ©2012 Author(s) CC Attribution 3.0 Unsuported License.","PeriodicalId":202276,"journal":{"name":"Soil Forming Factors and Processes from the Temperate Zone","volume":"53 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2012-12-08","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Soil Forming Factors and Processes from the Temperate Zone","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.15551/FPPZT.V11I1.466","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
位于cĂlmĂŢui和buzĂu河流域的盐碱地中的硒
测定了沿Călmăţui和buzuru山谷分布的salsodiols (Solonchaks和Solonetz)的A层硒含量。总硒含量在480 ~ 1140g·kg -1之间振荡,平均值为800g·kg -1。这一数值是世界非半胚土壤上层硒总含量的2.1倍。多布罗吉亚和罗马尼亚东南部平原的土壤中硒总含量分别为5.6和3.4倍。pH = 7时EDTA-CH3COONH4溶液中可溶的流动硒含量在13 ~ 25g·kg -1区间,平均值为18g·kg -1,是多布罗格亚土壤上层流动硒含量的4倍,是罗马尼亚平原东南部土壤流动硒含量的1.2倍。总硒含量与盐碱的一些理化性质之间建立了比例关系,并得到了统计上的保证。这些土壤的硒含量大多以钙、钠或镁(次生)硒酸盐的形式存在。不排除存在相同阳离子的亚硒酸盐。©2012作者CC Attribution 3.0不支持许可。
本文章由计算机程序翻译,如有差异,请以英文原文为准。