Gambelli Alberto Maria, Stornelli Giulia, Di Schino Andrea, Rossi Federico
Engineering Department, University of Perugia, Via G. Duranti 93, 06125 Perugia, Italy.
Industrial Engineering Department, University of Rome "Tor Vergata", Via del Politecnico 1, 00133 Rome, Italy.
Materials (Basel). 2021 Sep 6;14(17):5115. doi: 10.3390/ma14175115.
Hydrate formation and dissociation processes were carried out in the presence of a pure quartz porous medium impregnated with a metallic powder made with a CuSn12 alloy. Experiments were firstly made in the absence of that powder; then, different concentrations were added to the porous medium: 4.23 wt.%, 18.01 wt.%, and 30.66 wt.%. Then, the hydrate dissociation values were compared with those present in the literature. The porous medium was found to act as an inhibitor in the presence of carbon dioxide, while it did not alter methane hydrate, whose formation proceeded similarly to the ideal trend. The addition of CuSn12 promoted the process significantly. In particular, in concentrations of up to 18.01 wt.%, CO hydrate formed at milder conditions until it moved below the ideal equilibrium curve. For methane, the addition of 30.66 wt.% of powder significantly reduced the pressure required to form hydrate, but in every case, dissociation values remained below the ideal equilibrium curve.
水合物的形成和解离过程是在一种浸渍有由CuSn12合金制成的金属粉末的纯石英多孔介质存在的情况下进行的。实验首先在没有该粉末的情况下进行;然后,将不同浓度的粉末添加到多孔介质中:4.23重量%、18.01重量%和30.66重量%。然后,将水合物解离值与文献中的值进行比较。发现多孔介质在二氧化碳存在时起到抑制剂的作用,而它不会改变甲烷水合物,其形成过程与理想趋势相似。添加CuSn12显著促进了该过程。特别是,在浓度高达18.01重量%时,一氧化碳水合物在更温和的条件下形成,直到其移动到理想平衡曲线以下。对于甲烷,添加30.66重量%的粉末显著降低了形成水合物所需的压力,但在每种情况下,解离值仍低于理想平衡曲线。