木质素磺酸盐对火山灰反应合成产物的影响

Kanako Toda , Daisuke Minato , Takumi Saito , Ryosuke Kikuchi , Tsubasa Otake , Tsutomu Sato
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引用次数: 0

摘要

土壤有机质可以抑制火山灰反应,从而影响土用建筑材料的强度发展。为了了解它们之间的相互作用,本文以木质素磺酸盐为模型土壤有机质,通过批量试验研究了木质素磺酸盐对火山灰反应的影响。木质素磺酸盐抑制了火山灰反应,抑制了水合硅酸钙(C-S-H)的生成。随着木质素磺酸的加入,这种抑制不是连续发生的,而是在一定剂量的木质素磺酸时触发的。我们认为抑制作用主要是由于Si-(Ca)-木质素磺酸盐络合物的形成。这种相互作用可能说明了土壤中有机质在碱性活化下对火山灰反应的抑制作用。在阈值以下,木质素磺酸盐通过改变其结构允许C-S-H形成,这也表明在C-S-H形成共存的情况下,土壤有机质可能影响建筑材料的强度发展。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Effects of lignosulfonate on synthesis products of the pozzolanic reaction

Soil organic matters may inhibit the pozzolanic reaction, and thus influence the strength development of soil-employed construction materials. To understand their interaction, the effect of lignosulfonate, here used as model soil organic matter, on the pozzolanic reaction was investigated through batch experiments. Lignosulfonate inhibited the pozzolanic reaction, suppressing calcium silicate hydrate (C-S-H) formation. The suppression did not take place in a continuous way with the addition of lignosulfonate but was triggered at a certain dosage of lignosulfonate. We propose that the inhibition was primarily due to formation of Si-(Ca)-lignosulfonate complex. Such interaction may illustrate the inhibition of the pozzolanic reaction by organic matters in soils at alkaline activation. Below the threshold, lignosulfonate allowed C-S-H formation though modified its structure, which also suggested the possibility of soil organic matters to influence the strength development of construction materials in coexistence of C-S-H formation.

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