Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.2136/sssaj2010.0439 |
Distinguishing Boron Desorption from Mineral Dissolution in Arid-Zone Soils | |
Goldberg, Sabine; Suarez, Donald L. | |
通讯作者 | Goldberg, Sabine |
来源期刊 | SOIL SCIENCE SOCIETY OF AMERICA JOURNAL |
ISSN | 0361-5995 |
出版年 | 2011 |
卷号 | 75期号:4页码:1347-1353 |
英文摘要 | Boron release from six arid-zone soil samples from the San Joaquin Valley of California was investigated as a function of reaction time, solution pH, and suspension density. A multiple batch extraction experiment was performed for 362 d to distinguish B desorption from B released from mineral dissolution. Amounts of B released decreased rapidly and reached a low constant value aft er about 6 mo of reaction time. Slopes of the B release curves for the last eight extractions approached zero (constant release rate), indicating that this B release was from mineral dissolution. We also did a shorter term experiment that contained added Mg and silicate in solution. These experiments were conducted to evaluate the contribution of B release from dissolution of B-containing Mg silicate minerals. We determined that most of the B released from the soils can be attributed to release from sorption sites rather than resulting from dissolution of B-containing Mg silicates. Various B soil tests were evaluated for their ability to measure native extractable adsorbed B. The diethylenetriaminepentaacetic acid (DTPA)-sorbitol extract was the best measure of available adsorbed B but still only extracted 48% of the amount of B released in the long-term experiment. The greatest amount of B was extracted at the lowest suspension density for DTPA-sorbitol (92%) and phosphate buff er pH 6.6 (95%). These extractants are recommended for quantifying native extractable adsorbed B, which must be considered in application of chemical speciation transport models to describe B movement in soils. Incorporation of our results will allow improved predictions of soil solution B concentrations under diverse agricultural and environmental conditions. |
类型 | Article |
语种 | 英语 |
国家 | USA |
收录类别 | SCI-E |
WOS记录号 | WOS:000293076400015 |
WOS关键词 | PALYGORSKITE ; REGENERATION ; EQUILIBRIUM ; SERPENTINE ; CALIFORNIA ; SELENIUM ; BASIN ; AREA |
WOS类目 | Soil Science |
WOS研究方向 | Agriculture |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/170593 |
作者单位 | ARS, USDA, US Salin Lab, Riverside, CA 92507 USA |
推荐引用方式 GB/T 7714 | Goldberg, Sabine,Suarez, Donald L.. Distinguishing Boron Desorption from Mineral Dissolution in Arid-Zone Soils[J],2011,75(4):1347-1353. |
APA | Goldberg, Sabine,&Suarez, Donald L..(2011).Distinguishing Boron Desorption from Mineral Dissolution in Arid-Zone Soils.SOIL SCIENCE SOCIETY OF AMERICA JOURNAL,75(4),1347-1353. |
MLA | Goldberg, Sabine,et al."Distinguishing Boron Desorption from Mineral Dissolution in Arid-Zone Soils".SOIL SCIENCE SOCIETY OF AMERICA JOURNAL 75.4(2011):1347-1353. |
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