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首页> 外文期刊>Applied Geochemistry: Journal of the International Association of Geochemistry and Cosmochemistry >Environmental geochemistry significance of organic phosphorus: An insight from its adsorption on iron oxides
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Environmental geochemistry significance of organic phosphorus: An insight from its adsorption on iron oxides

机译:有机磷的环境地球化学意义:吸附氧化铁吸附的洞察

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Abstract Iron oxides in suspended particulate matter or bottom sediments can remove P from natural waters via sorption, rendering it unavailable for biological uptake. In this work, three dissolved OP compounds, were selected as adsorbents to investigate their adsorption behavior on two typical iron oxides. The results showed that the formation of nonprotonated and protonated bidentate complexes were the dominant mechanisms in the initial stage (~10?min) and the following stage (10–1440?min) during the adsorption process, respectively, in which the formation of protonated bidentate complex is the dominant mechanism in the whole adsorption process. Moreover, the adsorption density of P compounds on iron minerals increased with the temperature increase, indicating the endothermic and spontaneous of the adsorption process; pH presented negative effects on the adsorption of P-compounds on both hematite and goethite. Low molecular weight acid (LMWOAs) suppressed the adsorption of P compounds and the inhibitory effects increased with the number of carboxyl groups and the molecular size increasing. On the basis of this work, it can be deduced that P level will be largely elevated in water column from the WLSH-like lakes due to that the alkalization of water, the flourish of macrophyte and the icebound effects presented negative effects on P adsorption towards Fe oxyhydroxides in sediments. This work helps to interpret the knowledge linkage regarding the factors driving OP compounds behavior and bioavailability in lake ecosystem. Highlights ? The formation of nonprotonated bidentate complexes were the dominant mechanisms in the initial stage. ? While protonated bidentate complexes were the dominant after 10?min during the adsorption process. ? The inhibitory effects of LMWOAs increased with the increase of carboxyl groups and molecular size. ? P level will be largely elevated in water column from the WLSH-like lakes. ? It helps to interpret the factors driving OP compounds behavior and bioavailability. ]]>
机译:<![CDATA [ 抽象 悬浮颗粒物质或底部沉积物中的氧化铁可以通过吸附从天然水中除去P,使其无法用于生物学吸收。在这项工作中,选择三种溶解的OP化合物作为吸附剂,以研究其在两个典型的氧化铁上的吸附行为。结果表明,非普促和质子化的二齿复合物的形成是在吸附过程中初始阶段(〜10〜min)和以下阶段(10-1440〜min)中的显性机制,其中质子化的形成二齿复合物是整个吸附过程中的主导机制。此外,在铁矿物质上的P化合物的吸附密度随温度升高而增加,表明吸附过程的吸热和自发性; pH对赤铁矿和甲磺酸盐对P-化合物的吸附产生负面影响。低分子量酸(LMWOA)抑制了P化合物的吸附,抑制作用随羧基的数量和分子大小增加而增加。在这项工作的基础上,由于水的碱化,宏观物质的繁华和冰波效应,可以推断出P级,从WLS的湖泊的水柱中的水柱升高。沉积物中的Fe羟基氧化物。这项工作有助于解释关于在湖西生态系统中推动op化合物行为和生物利用度的因素的知识联系。 亮点 非普促的二齿复合物的形成是初始阶段中的主导机制。 在质子化的二齿复合物在吸附过程中10次占主导地位,在10?分钟后的主导。 Lmwoas的抑制作用随着羧基和分子大小的增加而增加。 P级将在WLSH类似的水柱中升高。湖泊。 它有助于解释驱动op化合物行为和生物利用度的因素。 ]]>

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