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Based on the conduit magma convection model, the relatively stable SO2 flux and gas composition indicate a stability of the magma plumbing and degassing conditions after March 2011, and the absence of eruptive activity since September 2011 may not readily indicate a decrease of the eruptive potential of the volcano.
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In this study, we investigate the effusive stage of the 2011 Shinmoe-dake eruption by means of numerical calculations based on the 1D steady conduit flow model.
To examine the conditions in the conduit and magma chamber, a numerical code is devised, based on the one-dimensional steady flow model of Kozono and Koyaguchi (2010), who modeled a dome-forming eruption.
The aim of this study was to investigate a new tubulization technique based on the employment of vein conduits filled with whole subcutaneous adipose tissue obtained by lipoaspiration.
We estimated the conduit radius based on the eruption rates of the preceding subplinian eruptions using Mastin's (2002) CONFLOW program.
We propose a new model of the response of spring discharge to rainfall based on the square law for turbulent conduit flow.
Continuity of the gastrointestinal tract should be restored with a gastric conduit based on the right gastric and gastroepiploic arteries.
The patients who underwent RC were subdivided based on the specific urinary diversion used: ileal conduit, continent cutaneous reservoir or orthotopic neobladder.
Based on the SO2 fluxes and the gas compositions, the conduit magma convection is considered as the gas supply mechanism at Shinmoedake, and the degassing pressure change is attributed to the change of depth of the convecting magma column top.
Based on the analysis results, the influence of turbulent conduit on the spring hydrograph from the point recharge is also discussed.
In this paper, the inadequacy of the power regression based model employed so far for estimating the normal depth in these conduits was presented based on the relative hydraulic sensitivity of structures.
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