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首页> 外文期刊>Journal of Environmental Radioactivity >Effect of K and bentonite additions on Cs-transfer to ryegrass
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Effect of K and bentonite additions on Cs-transfer to ryegrass

机译:钾和膨润土添加对Cs转移至黑麦草的影响

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摘要

Bentonite amendments are generally ineffective in reducing the soil-to-plant radiocaesium transfer but have previously been shown that bentonites in the K-form having been subjected to wetting-drying cycles had pronounced radiocaesium binding capacities. We have investigated the effect of wetting-drying (WD) on Radiocaesium Interception Potential (RIP) development in three K-bentonites and K-bentonite soil mixtures, using a variety of procedures: homogenisation of the bentonites with K through dialysis (K_B), or partial transformation of the bentonite to the K-form in the presence of a solution of K_2CO_3 (K_L) or in presence of solid K_2CO_3 (K_s). Of the three strategies tested, addition of K_2CO_3 (solid) at a dose of 2 meq g~(-1) clay and adding the K-bentonite mixtures to the soil resulted in the highest RIP increase after 20 WD cycles. The procedure giving the highest RIP yield is the most practical for further applications and was used in a pot experiment under greenhouse condition. When expressing the RIP increase of the soil-bentonite mixtures per unit bentonite added (RIP yield), 28-to 110-fold RIP increases were observed up to a value of ~60000 meq kg~(-1) (6 times higher than the RIP for illite). The beneficial effect following K-bentonite application was shown to be dependent both on a sorption enhancement effect (direct RIP effect) and fixation effects (indirect RIP effect). Greenhouse testing proved that the RIP effects observed in greenhouse could be predicted by making use of the sorption data from the laboratory tests. Optimum soil-amendment would be obtained with bentonites with high initial sorption RIP and a high sorption RIP increase when subjected to WD in the presence of potassium. Hypothised Transfer Factor (TF)-reductions of at least 10-fold could result when mixing ~1% bentonite, like Otay bentonite (RIP yield 99 000 meq kg~(-1) after WD in presence of K if only fine particle size of < 1 mm considered) with the contaminated ploughing layer.
机译:膨润土改性剂通常不能有效地减少土壤到植物的放射性铯的转移,但是以前已经证明,经过湿润干燥循环的K型膨润土具有显着的放射性铯结合能力。我们使用多种程序研究了湿干燥(WD)对三种K-膨润土和K-膨润土土壤混合物中放射性铯截留潜能(RIP)发展的影响,方法包括:通过透析将膨润土与K均质化(K_B),在存在K_2CO_3(K_L)溶液或存在固体K_2CO_3(K_s)的情况下,将膨润土部分或部分转化为K型。在所测试的三种策略中,以2 meq g〜(-1)粘土的量添加K_2CO_3(固体)并将K-膨润土混合物添加到土壤中,导致20 WD循环后RIP增幅最大。 RIP收率最高的程序对于进一步的应用是最实用的,并用于温室条件下的盆栽实验中。当表示每单位添加膨润土的土壤-膨润土混合物的RIP升高(RIP产量)时,观察到RIP升高了28到110倍,最高达到〜60000 meq kg〜(-1)(比土壤膨润土的高6倍)。 RIP(伊利石)。施用钾-膨润土后的有益作用显示出既依赖于吸附增强作用(直接RIP作用)又是固定作用(间接RIP作用)。温室测试证明,通过利用实验室测试中的吸附数据,可以预测温室中观察到的RIP效果。当在钾的存在下进行WD时,膨润土具有较高的初始吸附RIP和较高的吸附RIP增幅即可获得最佳的土壤改良剂。混合〜1%的膨润土时,至少会降低10倍的次生转移因子(TF),例如只有K的情况下,在K的情况下,WD后在K的情况下,Otay膨润土(RIP产量为99000 meq kg〜(-1))。考虑到小于1毫米的犁耕层)。

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