Handheld XRF Analyses of Two Veronese Paintings

2012 ◽  
pp. 51-73
Author(s):  
Erich Stuart Uffelman ◽  
Elizabeth Court ◽  
John Marciari ◽  
Alexis Miller ◽  
Lauren Cox
Keyword(s):  
Xrf Analyses ◽  
Handheld Xrf

scholarly journals Peran Kontaminasi Kerak pada Diferensiasi Magma Pembentuk Batuan Vulkanik Sungai Ampalas, Mamuju, Sulawesi Barat

EKSPLORIUM ◽  
2020 ◽  
Vol 41 (2) ◽  
pp. 73
Author(s):  
Windi Anarta Draniswari ◽  
Sekar Indah Tri Kusuma ◽  
Tyto Baskara Adimedha ◽  
I Gde Sukadana
Keyword(s):  
Magma Mixing ◽  
Volcanic Rocks ◽  
Geochemical Characteristics ◽  
X Ray ◽  
Radioactive Mineral ◽  
Alkaline Feldspar ◽  
High Alkalinity ◽  
Preliminary Study ◽  
Xrf Analyses

ABSTRAK Anomali radiometri telah ditemukan di area Sungai Amplas pada bongkah batuan vulkanik. Nilai yang terukur dari spektrometer gama adalah 787 ppm eU dan 223 ppm eTh. Penemuan ini menarik untuk pengembangan eksplorasi. Studi lebih lanjut diperlukan untuk mengetahui karekteristik batuan pembawa mineral radioaktif dari sampel in-situ. Penelitian ini bertujuan untuk mengetahui karakteristik petrologi dan geokimia batuan vulkanik Ampalas sebagai studi awal untuk mengetahui proses akumulasi mineral radioaktif pada batuan vulkanik Ampalas. Metodologi yang digunakan meliputi pengamatan lapangan, pengambilan sampel batuan, analisis petrografi dan X-Ray Fluorescence (XRF). Batuan vulkanik ampalas tersusun atas ponolit, foidit, dan foid-syenit. Tekstur batuannya terdiri dari porfiritik, aliran, rim piroksen, zoning, pseudo-leusit, korosi, inklusi mafik, dan sieve. Karakteristik geokimia menunjukkan alkalinitas tinggi dan indikasi pengayaan mineral radioaktif yang tersebar dalam batuan. Proses magmatis yang berperan dalam pembentukan batuan vulkanik adalah fraksionasi kristal (fraksionasi leusit dan alkali felspar), asimilasi kerak kontinen, dan pencampuran magma. Interaksi antara magma dan kerak menyebabkan diferensiasi magma berkelanjutan yang menghasilkan akumulasi uranium dan torium lebih tinggi.ABSTRACT Anomalous radiometry has been found in Ampalas River Area on volcanic rock boulder. The values measured from gamma spectrometer are 787 ppm eU and 223 ppm eTh. This discovery is promising for exploration development. Further study need to figure the radioactive mineral bearing rock characteristic from in-situ samples. The research aim is to determine the petrology and geochemical characteristics of Ampalas volcanic rocks as preliminary study to find radioactive mineral accumulation process of Ampalas volcanic rocks. The methodologies are field observation, rock sampling, petrography, and X-Ray fluorescence (XRF) analyses. The Ampalas volcanic rocks consist of phonolite, phoidite, and phoid syenite. Their textures are porphyritic, flow, pyroxene rim, zoning, pseudo-leucite, corrosion, mafic inclusions, and sieve. The geochemical characteristics show high alkalinity and radioactive mineral enrichment disseminating on rock. The magmatic processes which play a significant role in radioactive mineral-bearing rocks formation are crystal fractionations (leucite and alkaline feldspar fractionations), continental crust assimilation, and magma mixing. Long interaction between magma and crust creates advanced magma differentiation causing higher uranium and thorium accumulation.  

scholarly journals Study on Western Asiatic cast ribbed rectangular beads from Kaman-Kalehöyük, Turkey, by using portable X-ray fluorescence

2013 ◽  
Vol 1 (1) ◽  
pp. 23
Author(s):  
Izumi Nakai ◽  
Kriengkamol Tantrakarn ◽  
Yoshinari Abe ◽  
Sachihiro Omura
Keyword(s):  
Bronze Age ◽  
Principal Component ◽  
Glass Beads ◽  
Late Bronze Age ◽  
Ancient Trade ◽  
Western Asia ◽  
Material Evidence ◽  
Excavation Site ◽  
Plant Ash ◽  
Xrf Analyses

In this article we report a comparative study on excavated objects and artifact from museums to reveal an aspect of ancient trade. The target artifact is Western Asiatic cast ribbed rectangular beads excavated from an architectural remain at Kaman-Kalehöyük, Turkey. Blue glass beads of this type have been excavated in Western Asia from north Iran and Iraq to the Syro-Palestinian coast from second half of 16th to 14th century BC. The analysis of the samples was carried out by using a portable Xray fluorescence (XRF) spectrometer developed by us. The instrument was brought to the excavation site in Turkey as well as to the museums to analyse typologically similar glass beads from the collection of Okayama Orient Museum and MIHO MUSEUM in Japan, for comparison. Our XRF analyses suggested that all analysed glass artifacts are plant ash sodalime silica glass with 2-4 wt% magnesium and potassium. The three glass beads exhibited similar compositional characteristic, i.e. they contain Sb, Pb, Fe, Cu and Sr in similar quantities. A typological and principal component analysis comparison of the glass beads unearthed from Kaman- Kalehöyük site with those of the museums and literature data support that they should have a similar origin. In addition, archaeological context of the glass from Kaman-Kalehöyük also supports that the artifact belongs to the Middle-Late Bronze Age (16th to 15th centuries BC). This is the first scientific material evidence that shows the possibility of a cultural flow from Mesopotamia region to Kaman-Kalehöyük during Middle- Late Bronze Age.

Testing the analytical performance of handheld XRF using marine sediments of IODP Expedition 355

2019 ◽  
Vol 157 (6) ◽  
pp. 956-960 ◽  
Author(s):  
A. Hahn ◽  
M. G. Bowen ◽  
P. D. Clift ◽  
D. K. Kulhanek ◽  
M. W. Lyle
Keyword(s):  
Standard Procedure ◽  
Quality Data ◽  
Geochemical Data ◽  
Stratigraphic Correlation ◽  
Common Denominator ◽  
Handheld Device ◽  
Xrf Analysis ◽  
Xrf Scanning ◽  
International Ocean Discovery Program ◽  
Handheld Xrf

AbstractObtaining geochemical profiles using X-ray fluorescent (XRF) techniques has become a standard procedure in many sediment core studies. The resulting datasets are not only important tools for palaeoclimatic and palaeoceanographic reconstructions, but also for stratigraphic correlation. The International Ocean Discovery Program (IODP) has therefore recently introduced shipboard application of a handheld XRF device, making geochemical data directly available to the science party. In all XRF scanning techniques, the physical properties of wet core halves cause substantial analytical deviations. In order to obtain estimates of element concentrations (e.g. for quantitative analyses of fluxes or mass-balance calculations), a calibration of the scanning data is required. We test whether results from the handheld XRF analysis on discrete samples are suitable for calibrating scanning data. Log-ratios with Ca as a common denominator were calculated. The comparison between the handheld device and conventional measurements show that the latter provide high-quality data describing Al, Si, K, Ca, Ti, Mn, Fe, Zn, Rb and Sr content (R2 compared with conventional measurements: ln(Al/Ca) = 0.99, ln(Si/Ca) = 0.98, ln(K/Ca) = 0.99, ln(Ti/Ca) = 0.99, ln(Mn/Ca) = 0.99, ln(Fe/Ca) = 0.99, ln(Zn/Ca) = 0.99 and ln(Sr/Ca) = 0.99). Our results imply that discrete measurements using the shipboard handheld analyser are suitable for the calibration of XRF scanning data. Our test was performed on downcore sediments from IODP Expedition 355 that display a wide variety of lithologies of both terrestrial and marine origin. The implication is that our findings are valid on a general scale and that shipboard handheld XRF analysis on discrete samples should be used for calibrating XRF scanning data.

Utilization of dried sludge for making ceramsite

2006 ◽  
Vol 54 (9) ◽  
pp. 69-79 ◽  
Author(s):  
G.R. Xu ◽  
J.L. Zou ◽  
Y. Dai
Keyword(s):  
Municipal Wastewater ◽  
Solid Phase ◽  
Particle Density ◽  
Raw Material ◽  
Solid Phase Reaction ◽  
Phase Reaction ◽  
Sintering Process ◽  
Sintering Time ◽  
Dried Sludge ◽  
Xrf Analyses

Dried sludge as additive for making ceramsite is a new effective approach for disposal of sludge. In this study sewage sludge, water glass and clay were chosen as the components, the optimal ratio of the components and the most appropriate conditions were obtained. The functions of primary components in the sintering process, porosity formation mechanism and solid phase reaction also have been discussed. The optimized process parameters were shown as follows: the ratio of dried sludge /clay (wt%) was 33%, ratio of adherent /clay (wt%) was 15%, sintering temperature was 1000 °C, sintering time was 10 min. Bulk density was 582 kg m−3, particle density was 1,033 kg m−3, water absorption was 9.5%, porosity was 43.7%. SEM, EDS, XRD and XRF analyses were also carried out. The results indicate that dried sludge as raw material is a good way for making ceramsite. Biological Aerated Filters (BAFs) with filter media of Guangzhou ceramsite, Jiangxi ceramsite, activated carbon and ceramsite (obtained in test) were selected to treat municipal wastewater. The average removal efficiencies of ceramsite (obtained in test) for turbidity, COD, SCOD and NH3-N were about 96.4%, 76.2%, 59.6% and 82.3% respectively and were higher than those of other ceramsites.

Evaluation of the utility of handheld XRF in meteoritics

2011 ◽  
Vol 40 (6) ◽  
pp. 449-463 ◽  
Author(s):  
Florian J. Zurfluh ◽  
Beda A. Hofmann ◽  
Edwin Gnos ◽  
Urs Eggenberger
Keyword(s):  
Handheld Xrf

scholarly journals Obsidian from the Site of Piano dei Cardoni, Ustica (Palermo, Italy): Preliminary Results on the First Occupation of the Island

2021 ◽  
Vol 7 (1) ◽  
pp. 273-290
Author(s):  
Claudia Speciale ◽  
Kyle P. Freund ◽  
Sandro de Vita ◽  
Nunzia Larosa ◽  
Vincenza Forgia ◽  
...  
Keyword(s):  
Raw Material ◽  
Human Occupation ◽  
Late Neolithic ◽  
Field Surveys ◽  
Lithic Assemblage ◽  
Material Sources ◽  
Southern Side ◽  
Ams Dating ◽  
First Time ◽  
Xrf Analyses

Abstract New investigations on Ustica (Palermo, Sicily) originated from the need to improve our knowledge of the island’s archaeological and environmental heritage. Through field surveys, particular attention was paid to human occupation in the Neolithic phases and focused on the less investigated southern side of the island. The systematic survey of the area of Piano dei Cardoni in 2018 brought to light a new Middle/Late Neolithic site, already partially documented in the literature. The island was settled for the first time during these phases, as also testified from the area of Punta Spalmatore. The presence of Serra d’Alto, incised dark burnished, and Diana styles suggests that the site and the archaeological assemblage dates from the mid to late 5th millennium BC, as confirmed by AMS dating. In addition to pottery, obsidian artifacts were also recovered, and a preliminary study of these materials is presented here. Portable XRF analyses on a sample of 41 obsidian artifacts, representing a high percentage of the lithic assemblage compared to chert tools, show that the provenance of the raw material is Gabellotto Gorge (Lipari) and Balata dei Turchi (Pantelleria). These results provide new insight into broader regional debates about obsidian technology and its exchange during the Neolithic and open an important consideration for sites that are far from the raw material sources.

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