Kristalinitas Abu Vulkanik Gunung Soputan dan Implikasinya Terhadap Perilaku Eksplosif pada Erupsi Tahun 2016 dan 2018

Gunung Soputan adalah gunung basaltik dengan tipe erupsi eksplosif. Tipikal eksplosif berkaitan dengan karakter magma. Penelitian ini bertujuan untuk mengkaji kristalinitas abu vulkanik Gunung Soputan tahun 2016 dan 2018 dan implikasinya terhadap perilaku eksplosifnya. Kristalinitas abu vulkanik dikarakterisasi menggunakan peralatan difraktometer sinar X. Indeks kristalinitas dikalkulasi menggunakan persamaan Soltys dan ukuran kristal dikomputasi dengan persamaan Debye-Scherrer. Morfologi partikel abu dikarakterisasi menggunakan SEM. Hasil karakterisasi menunjukkan bahwa abu Soputan tahun 2016 dan 2018 memiliki indeks kristalinitas yang tinggi dan mengandung sejumlah kristal berukuran kecil serta memiliki dua bentuk morfologi yaitu bentuk padat dan blok bervesikular untuk abu hasil erupsi 4 Januari 2016, dan bentuk padat dan blok untuk abu hasil erupsi 6 Februari 2016 dan 3 Oktober 2018. Kristalinitas yang tinggi menyebabkan magma Soputan memiliki viskositas yang memadai untuk terjadinya erupsi yang eksplosif. Karakter eksplosif Gunung Soputan terekam dalam morfologi abu vulkaniknya.Kata kunci: Abu vulkanik; erupsi eksplosif; fragmentasi getas; indeks kristalinitasCristallinity of Volcanic Ash of Mount Soputan and Its Implication to Explosive Behaviour on Eruption of 2016 and 2018ABSTRACTMount Soputan is a basaltic mountain with an explosive eruption type. Typical explosives relate to the character of the magma. This study aims to examine the crystallinity of Mount Soputan's volcanic ash in 2016 and 2018 and its implications for its explosive behavior. The crystallinity of volcanic ash was characterized using an X-ray diffractometer. The crystallinity index was calculated using the Soltys equation and the crystal size computed using the Debye-Scherrer equation. The morphology of the ash particles was characterized using SEM. The characterization results show that the 2016 and 2018 Soputan ash has a high crystallinity index and contains a number of small crystals and has two morphological forms, namely solid form and vesicular block for ash from the eruption on January 4, 2016, and solid and block form for eruption ash 6 February 2016 and October 3 2018. High crystallinity causes the Soputan magma to have sufficient viscosity for explosive eruptions. The explosive character of Mount Soputan is recorded in the morphology of its volcanic ash.Keywords: Brittle fragmentation; crystallinity index; explosive eruption; volcanic ash

Experimental and microstructure analysis of the penetration resistance of composite structures

Composite structures (SiC/UHMWPE/TC4; SiC/TC4/UHMWPE) were designed using silicon carbide (SiC)ceramics, ultra-high-molecular-weight polyethylene (UHMWPE) laminate, and titanium alloys (TC4s). Penetration experiments and numerical simulations were carried out to study the anti-penetration mechanism and energy characteristics of the composite structures, and the microstructure of the TC4 was analyzed. The results show that the two composite structures designed have advantages in reducing mass and thickness. The energy proportion of the TC4 is the largest among the three materials, which mainly determines the anti-penetration performance. The microstructure of the TC4 in composite structure I shows rough edges of bullet holes, a large number of adiabatic shear bands (ASBs), ASB bends and bifurcates, and many cracks, which lead to spalling damage of the TC4. The microstructure of the TC4 in composite structure II shows flat edges of bullet holes, several straight ASBs, and no cracks, which leads to brittle fragmentation. The initiation, expansion, combination of ASBs and cracks lead to more energy consumption. Therefore, the combination form of composite structure I can give full play the energy dissipation mechanism of the TC4 and has better anti-penetration performance than composite structure II.

Melting and fragmentation laws from the evolution of two large Southern Ocean icebergs estimated from satellite data

The evolution of the thickness and area of two large Southern Ocean icebergs that have drifted in open water for more than a year is estimated through the combined analysis of altimeter data and visible satellite images. The observed thickness evolution is compared with iceberg melting predictions from two commonly used melting formulations, allowing us to test their validity for large icebergs. The first formulation, based on a fluid dynamics approach, tends to underestimate basal melt rates, while the second formulation, which considers the thermodynamic budget, appears more consistent with observations. Fragmentation is more important than melting for the decay of large icebergs. Despite its importance, fragmentation remains poorly documented. The correlation between the observed volume loss of our two icebergs and environmental parameters highlights factors most likely to promote fragmentation. Using this information, a bulk model of fragmentation is established that depends on ocean temperature and iceberg velocity. The model is effective at reproducing observed volume variations. The size distribution of the calved pieces is estimated using both altimeter data and visible images and is found to be consistent with previous results and typical of brittle fragmentation processes. These results are valuable in accounting for the freshwater flux constrained by large icebergs in models.

Melting and fragmentation laws from the evolution of two large southern ocean icebergs

The evolution of the thickness and area of two large southern ocean icebergs, having drifted in open water for more than a year, is estimated through the combined analysis of altimeter data and visible satellite images. Most of the iceberg modelling studies uses two main melting formulations that are compared with the observed thickness evolution of our two icebergs, to test their validity in case of large icebergs. The first formulation, based on a fluid dynamics approach, would tend to underestimate basal melt rates, so that using the second one (using a thermodynamic budget consideration) may be more relevant. Fragmentation is, before melting, the major decay process of large icebergs, yet it is a complex and still poorly documented mechanism. A correlation analysis between the observed volume loss of our two icebergs and environmental parameters highlights those most likely to promote fragmentation. Consequently, a bulk model of fragmentation depending on ocean temperature and iceberg velocity is established and is shown to be able to reproduce well the observed volume variations. Finally, the size distribution of the calved pieces is estimated using both altimeter data and visible images and is found to be consistent with previous studies as typical of brittle fragmentation processes. These results are valuable to account for a more realistic representation of the freshwater flux constrained by large icebergs in models.

Analisis Tipikal Erupsi Gunung Lokon Periode Erupsi 2012-2013 Berdasarkan Karakterisasi Mikrostruktur Abu Vulkanik

Gunung Lokon yang berada di lengan utara Sulawesi adalah salah satu gunung api paling aktif di Indonesia. Perilaku erupsinya telah dipelajari melalui analisis mikrostruktur abu vulkanik. Tujuan dari karakterisasi mikrostruktur adalah untuk mengestimasi nilai dari viskositas dan permeabilitas magma. Karakterisasi mikrostruktur menggunakan XRD, FTIR, SEM/EDS/XRF dan µCT. Abu vulkanik Lokon adalah mineral polimorf yang banyak mengandung kristal plagioklase. Abu Lokon mempunyai kandungan air 0,3 -0,6 % berat dan massa dasarnya terdiri dari partikel vesikular dan non vesikular. Viskositas dari magma Lokon adalah sekitar 107Pa.s pada 10000C dan fraksi volume kristal sekitar 0,45-0,5. Hasil-hasil ini menunjukkan bahwa reologi magma Lokon adalah bersifat non Newtonian dan mekanisme fragmentasinya adalah brittle fragmentation. Berdasarkan pada permeabilitas dan porositas yang dikuantisasi dengan µCT dapat disimpulkan bahwa fragmentasi magmanya tidak dipicu oleh outgassing. Dinamika erupsi eksplosif dari Gunung Lokon pada 2012-2013 adalah erupsi vulkanian pada skala sedang.Lokon volcano where located on North arm of Sulawesi is one of the most active volcanoes in Indonesia. Behaviour of its eruptions have been learned through microstructure analysis of volcanic ash. The goal of microstructure characterization is estimate value of magma viscosity and permeability. Characterization of microstructure using XRD, FTIR, SEM/EDS/XRF and µCT. Lokon volcanic ash is a polymorph minerals which contains many plagioclase crystal. Ash has water content between 0.3 – 0.6 % wt and its groundmass contains vesicular and non vesicular particles. Viscosity of Lokon magma is about 107Pa.s at 10000C and fraction of crystal volum between 0.45-0.5. These results showed that magma rheology of Lokon is non Newtonian and the mechanism of its fragmentation is brittle fragmentation. Based on permeability and porosity that quantified by µCT, it is concluded that the brittle fragmentation is not triggered by outgassing. Dynamics of explosive eruption of Lokon volcano at 2012-2013 is moderate vulcanian eruption.

Fault rheology beyond frictional melting

During earthquakes, comminution and frictional heating both contribute to the dissipation of stored energy. With sufficient dissipative heating, melting processes can ensue, yielding the production of frictional melts or “pseudotachylytes.” It is commonly assumed that the Newtonian viscosities of such melts control subsequent fault slip resistance. Rock melts, however, are viscoelastic bodies, and, at high strain rates, they exhibit evidence of a glass transition. Here, we present the results of high-velocity friction experiments on a well-characterized melt that demonstrate how slip in melt-bearing faults can be governed by brittle fragmentation phenomena encountered at the glass transition. Slip analysis using models that incorporate viscoelastic responses indicates that even in the presence of melt, slip persists in the solid state until sufficient heat is generated to reduce the viscosity and allow remobilization in the liquid state. Where a rock is present next to the melt, we note that wear of the crystalline wall rock by liquid fragmentation and agglutination also contributes to the brittle component of these experimentally generated pseudotachylytes. We conclude that in the case of pseudotachylyte generation during an earthquake, slip even beyond the onset of frictional melting is not controlled merely by viscosity but rather by an interplay of viscoelastic forces around the glass transition, which involves a response in the brittle/solid regime of these rock melts. We warn of the inadequacy of simple Newtonian viscous analyses and call for the application of more realistic rheological interpretation of pseudotachylyte-bearing fault systems in the evaluation and prediction of their slip dynamics.