cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.14457/tu.the.2021.1257
title: การศึกษาผลกระทบจากแรงแผ่นดินไหวต่อถังกักเก็บของเหลวหน้าตัดรูปวงกลม

description: ถังกักเก็บของเหลวหน้าตัดรูปวงกลมขนาดใหญ่เป็นหนึ่งในโครงสร้างพื้นฐานที่สำคัญในกิจการการประปา ในประเทศไทยโครงสร้างดังกล่าวจำนวนมากถูกก่อสร้างมาก่อนที่จะมีการเริ่มใช้ข้อบังคับที่เกี่ยวข้องกับการออกแบบอาคารเพื่อต้านทานแผ่นดินไหว งานวิจัยนี้มีวัตถุประสงค์เพื่อศึกษาผลกระทบจากแรงสั่นสะเทือนเนื่องจากแผ่นดินไหวต่อถังกักเก็บของเหลวหน้าตัดรูปวงกลมดังกล่าว โดยการศึกษานี้แบ่งออกเป็น 2 ส่วน ส่วนที่ 1 เป็นการวิเคราะห์โครงสร้างเพื่อหาแรงที่เกิดขึ้นเนื่องจากการกระเพื่อของของเหลว (Sloshing) จากแรงสั่นสะเทือนเนื่องจากแผ่นดินไหว โดยใช้โปรแกรมที่มีความสามารถในการวิเคราะห์ทางไฟไนต์วอลุม (Finite Volume Method, FVM) คู่ควบกับวิธีไฟไนต์เอลิเมนต์ (Finite Element Method, FEM) ทำการจำลองโครงสร้างในรูปแบบ 3 มิติ เพื่อศึกษาและวิเคราะห์แรงที่เกิดขึ้นจากการกระเพื่อมของของเหลว (Sloshing) และถ่ายแรงกระเพื่อมดังกล่าวสู่โครงสร้างโดยใช้ Penalty Contact Algorithm ทำการจำลองโครงสร้างในส่วนของเสาให้เป็นแบบเสาเดี่ยวที่มีสติฟเนสเทียบเท่า (Equivalent Stiffness) เท่ากับเสาของถังตกตะกอนที่ทำการศึกษา ส่วนที่ 2 วิเคราะห์ผลของแรงที่เกิดขึ้นเนื่องจากการกระเพื่อมของของเหลว (Sloshing) กับโครงสร้างโครงสร้าง โดยวิธีประวัติเวลาในช่วงพิกัดยืดหยุ่น สำหรับข้อมูลคลื่นแผ่นดินไหวที่ใช้ในการวิเคราะห์นั้น เป็นข้อมูลประวัติเวลาความเร่งของพื้นดิน (Ground Acceleration Time History) ตามมาตรฐานการออกแบบอาคารต้านทานการสั่นสะเทือนของแผ่นดินไหว (มยผ. 1301/1302-61) ในพื้นที่โซน 5 โดยใช้คลื่นแผ่นดินไหวที่ผิวดินที่คาบการสั่นของอาคารเท่ากับ 0.2 วินาที 0.5 วินาที และ 3.0 วินาที ซึ่งการศึกษานี้เป็นการประยุกต์ใช้การวิเคราะห์ทางไฟไนต์วอลุมเพื่อถ่ายแรงเนื่องจากการกระเพื่อมของของเหลว (Sloshing) สู่เสาเดี่ยวที่มีสติฟเนสเทียบเท่า (Equivalent Stiffness) เพื่อประเมินโครงสร้างในการต้านทานแรงสั่นสะเทือนอันเนื่องมาจากแผ่นดินไหว
DOI: 10.5285/256981dc-245b-410a-90a4-5f0138583a65
title: Effect of porosity and clays on geophysical and transport properties of sandstone exposed to CO2 injection: Influence of rock heterogeneities on CO2 storage monitoring

description: This dataset gathers the data collected during a brine:CO2 flow-through experiments conducted on three sandstones with similar mineralogical compositions (major minerals) but different porosity, clay-size fraction and clay mineralogy. The aim was to study the effect of such heterogeneities on interpretation of geophysical data. Geophysical and transport data were collected before, during and after exposing each sample to CO2, and analysed with basic petrophysical properties. 
The tests were conducted in the high-pressure, room-temperature (20°C) experimental setup for multi-flow-through tests in the Rock Physics Laboratory at the National Oceanography Centre, Southampton (NOCS), during 2022, as part of the OASIS, EHMPRES and FOCUS projects with funding from the Research Council of Norway (RCN grant no. 280472 - OASIS) and the Natural Environment Research Council (NERC grants NE/X003248/1 - FAPESP-EHMPRES, and NE/X006271/1 - FOCUS). 
To simulate the specific effective stress conditions of the target CO2 storage reservoir in Aurora (Aker et al., 2021), northern North Sea, the confining and pore pressure conditions of the reservoir were accommodated to our lab  temperature conditions. We measured ultrasonic P- and S-wave velocities and attenuations, axial strains and electrical resistivity for an increasing CO2 saturation. The degree of brine saturation was inferred from the electrical resistivity using the modified Archie’s empirical relationship to account for the contribution of clay minerals, based on the Waxman–Smits–Juhasz model (see further details in, e.g., Falcon-Suarez et al. (2021)). We refer to Falcon-Suarez et al. (2020) for further information about the experimental rig and the CO2 injection protocol.
DOI: 10.6084/m9.figshare.24512899
title: Women who submitted papers to the Royal Society after 1853: a sample

description: The first papers by women known to be published by the Royal Society are those by Caroline Herschel (1786) and Mary Somerville (1826) - though a letter by Ann Savile had appeared within a paper by Tancred Robinson in 1696.The list in this spreadsheet provides some insight into the women who submitted papers to the Royal Society of London after Herschel and Somerville. It has been generated from a partial transcription of the Royal Society's 'Register of Papers', undertaken by Aileen Fyfe's project team at the University of St Andrews.The Register of Papers begins in 1853, and records all papers SUBMITTED to the Society's journals, the Philosophical Transactions and the Proceedings. We transcribed all entries fronm 1853 to 1890, and thereafter transcribed two sample years per decade (ending in -0 and -5). This is NOT a list of all women authors at the Royal Society: it records the names of authors who SUBMITTED papers to the Royal Society's journals during the transcribed SAMPLE years. It gives a good indication of all women authors in the late 19thC, but is simply an illustrative sample for the 20thC<b>Caveats</b>The Register of Papers starts in 1853. We transcribed everything from 1853 to 1890. Thereafter, everything in two sample years per decade, ending in -0 and -5.Not all of these submitted papers were approved for publicationAttribution of gender was done retrospectively by our team, based on the presence of titles (e.g. Miss, Mrs) or by human recognition of forenames. There may be more women authors out there (e.g. hidden behind initials)The list is organised to show unique women authors - so if two women co-authored a paper, there are two entries for a single paper (one for each woman author)Year = year of submission of paper to RS, not necessarily year of publicationAll papers had to be submitted by a Fellow (until 1990), so if there was no Fellow as co-author, there had to be a Fellow acting as 'communicator' (all Fellows were male until 1945)Author 'identifiers' are (where possible) the Royal Society's fellows identifiers (starting NA…)
DOI: 10.6084/m9.figshare.24512899.v1
title: Women who submitted papers to the Royal Society after 1853: a sample

description: The first papers by women known to be published by the Royal Society are those by Caroline Herschel (1786) and Mary Somerville (1826) - though a letter by Ann Savile had appeared within a paper by Tancred Robinson in 1696.The list in this spreadsheet provides some insight into the women who submitted papers to the Royal Society of London after Herschel and Somerville. It has been generated from a partial transcription of the Royal Society's 'Register of Papers', undertaken by Aileen Fyfe's project team at the University of St Andrews.The Register of Papers begins in 1853, and records all papers SUBMITTED to the Society's journals, the Philosophical Transactions and the Proceedings. We transcribed all entries fronm 1853 to 1890, and thereafter transcribed two sample years per decade (ending in -0 and -5). This is NOT a list of all women authors at the Royal Society: it records the names of authors who SUBMITTED papers to the Royal Society's journals during the transcribed SAMPLE years. It gives a good indication of all women authors in the late 19thC, but is simply an illustrative sample for the 20thC<b>Caveats</b>The Register of Papers starts in 1853. We transcribed everything from 1853 to 1890. Thereafter, everything in two sample years per decade, ending in -0 and -5.Not all of these submitted papers were approved for publicationAttribution of gender was done retrospectively by our team, based on the presence of titles (e.g. Miss, Mrs) or by human recognition of forenames. There may be more women authors out there (e.g. hidden behind initials)The list is organised to show unique women authors - so if two women co-authored a paper, there are two entries for a single paper (one for each woman author)Year = year of submission of paper to RS, not necessarily year of publicationAll papers had to be submitted by a Fellow (until 1990), so if there was no Fellow as co-author, there had to be a Fellow acting as 'communicator' (all Fellows were male until 1945)Author 'identifiers' are (where possible) the Royal Society's fellows identifiers (starting NA…)
DOI: 10.6084/m9.figshare.24524302
title: MAG nucleotides

description: Nucleotide sequences for the 14 new MAGs described in this study.
DOI: 10.6084/m9.figshare.24524302.v1
title: MAG nucleotides

description: Nucleotide sequences for the 14 new MAGs described in this study.
DOI: 10.15468/9bzedq
title: Morphological trends and genetic divergence in anacondas, genus Eunectes Wagler, 1830 (Serpentes: Boidae)

description: This dataset contains the digitized treatments in Plazi based on the original journal article Tarkhnishvili, David, Hille, Axel, Waller, Thomas, Todua, Mariam, Murtskhvaladze, Marine, Böhme, Wolfgang (2022): Morphological trends and genetic divergence in anacondas, genus Eunectes Wagler, 1830 (Serpentes: Boidae). Amphibia-Reptilia 43 (4): 379-393, DOI: 10.1163/15685381-bja10114
DOI: 10.5281/zenodo.10081590
title: Shear-wave splitting measurements in the Dead Sea rift
DOI: 10.5281/zenodo.10081589
title: Shear-wave splitting measurements in the Dead Sea rift
DOI: 10.3886/e195001
title: The Geography of Principal Internships in North Carolina

description: Principal preparation programs play an important role in developing future school leaders’ skills and practices. Internships, or structured opportunities for future leaders to engage in the work of school leadership in hands-on, authentic ways are among the most essential components of principal preparation. Using longitudinal data from 12 programs in North Carolina, this study extends research on internships by examining the pathways of interns from prior- to post-internship employment. We find that internships are highly localized around interns’ prior- and post-employment schools, but not their preparation program, with wide variability in placements between programs. Interns’ demographics do not play a large role in shaping the geography of internship placements. However, we find that preparation program type is strongly related to the geography of internship placements, suggesting that differences in program structure may shape internship placements. We conclude by highlighting the limitations and discussing implications for future research.
DOI: 10.3886/e195001v1
title: The Geography of Principal Internships in North Carolina

description: Principal preparation programs play an important role in developing future school leaders’ skills and practices. Internships, or structured opportunities for future leaders to engage in the work of school leadership in hands-on, authentic ways are among the most essential components of principal preparation. Using longitudinal data from 12 programs in North Carolina, this study extends research on internships by examining the pathways of interns from prior- to post-internship employment. We find that internships are highly localized around interns’ prior- and post-employment schools, but not their preparation program, with wide variability in placements between programs. Interns’ demographics do not play a large role in shaping the geography of internship placements. However, we find that preparation program type is strongly related to the geography of internship placements, suggesting that differences in program structure may shape internship placements. We conclude by highlighting the limitations and discussing implications for future research.
DOI: 10.5281/zenodo.10079592
title: Laser interferometry measurements of a Moroccan rabāb

description: Instrument: rabāb Country of origin: Morocco Place of origin: Fès Instrument maker: Abdessalam Chiki Year of manufacture: 2015 Location: Basel, private property of Thilo Hirsch
Dimensions: Total length: 513.2 mm Max. Body width: 114.8 mm Width at the upper end of the skin: 96.2 mm Width at top nut: 31.6 mm Body depth at the upper end of the skin: approx. 80 mm
Vibrating string lengths: d-string: 410 mm G-string: 403 mm
Materials: Body: walnut Pegbox: walnut Fingerboard: Acajou (mahogany) Decoration: mother-of-pearl Bars: spruce Top nut, tailpiece button: Bone Bridge: bamboo Top: goatskin
Laser interferometry measurements: Alexander Mayer, mdw - University of Music and Performing Arts Vienna, Department of Music Acoustics – Wiener Klangstil (IWK), 18.2.2020
Each figure (Filenames: A_####Hz.jpg) corresponds to the frequency of excitation on the bass side of the bridge (shaker: Frederiksen Vibration Generator Nr 2185.00). Images are made by time-averaging of laser speckle interference at the camera (time-average ESPI approach). Operating deflection shapes (roughly translating to theoretical vibrating modes) are observed at each frequency.
Photo of the setup: Thilo Hirsch
DOI: 10.21942/uva.24524338
title: Data and analysis package.zip

description: Raw Data. analysis tools etc
DOI: 10.21942/uva.24524338.v1
title: Data and analysis package.zip

description: Raw Data. analysis tools etc
DOI: 10.6084/m9.figshare.24524750.v1
title: Appendix A: The Bowland Shale Formation in the Blacon Basin: syngenetic processes, stacking patterns and heat productivity

description: Appendix A: discrete sample geochemical datasets (RockEval pyrolysis, XRF elemental analysis, stable C and S isotopes).
DOI: 10.6084/m9.figshare.24524750
title: Appendix A: The Bowland Shale Formation in the Blacon Basin: syngenetic processes, stacking patterns and heat productivity

description: Appendix A: discrete sample geochemical datasets (RockEval pyrolysis, XRF elemental analysis, stable C and S isotopes).
DOI: 10.6084/m9.figshare.24306493
title: <i>Wickerhamiella koratensis</i> sp. nov. and <i>Wickerhamiella limtongiae</i> sp. nov. - <i>de novo</i> assembly

description: Phylogenomic delineation of two new species of ascomycetous yeasts - <i>Wickerhamiella koratensis</i> sp. nov. and <i>Wickerhamiella limtongiae</i> sp. nov. - and proposal of two synonyms - <i>Wickerhamiella infanticola</i> and <i>Wickerhamiella tropicalis.</i>
DOI: 10.6084/m9.figshare.24524816
title: Appendix A: The Bowland Shale Formation in the Blacon Basin: syngenetic processes, stacking patterns and heat productivity

description: Appendix A: discrete sample geochemical datasets (RockEval pyrolysis, XRF elemental analysis, stable C and S isotopes).
DOI: 10.6084/m9.figshare.24524816.v1
title: Appendix A: The Bowland Shale Formation in the Blacon Basin: syngenetic processes, stacking patterns and heat productivity

description: Appendix A: discrete sample geochemical datasets (RockEval pyrolysis, XRF elemental analysis, stable C and S isotopes).
DOI: 10.5281/zenodo.10079956
title: Transfer function measurements of a Moroccan rabāb

description: Instrument: rabāb Country of origin: Morocco Place of origin: Fès Instrument maker: Abdessalam Chiki Year of manufacture: 2015 Location: Basel, private property of Thilo Hirsch
Dimensions: Total length: 513.2 mm Max. Body width: 114.8 mm Width at the upper end of the skin: 96.2 mm Width at top nut: 31.6 mm Body depth at the upper end of the skin: approx. 80 mm
Vibrating string lengths: d-string: 410 mm G-string: 403 mm
Materials: Body: walnut Pegbox: walnut Fingerboard: acajou (mahogany) Decoration: mother-of-pearl Bars: spruce Top nut, tailpiece button: bone Bridge: bamboo Top: goatskin
Transfer function measurements: Alexander Mayer, mdw - University of Music and Performing Arts Vienna, Department of Music Acoustics – Wiener Klangstil (IWK), 18.2.2020
Transfer function from shaker to microphone 1 meter in front of the instrument. Frequency range specified in the Filename. Shaker exciting with a frequency sweep on the bass side of the bridge (shaker type: Minishaker by BNK). Pressure measurement with a ROGA RG50 microphone.
Photos of the setup: Thilo Hirsch 18.2.2020
________________________
How to read VIA-Files: Line 1 to 9: Header, Line 8 holds the number of values Data is organized as followed: 1st col: Frequency [Hz]          2nd col: Magnitude [as Factor not dB!]        3rd col: Phase [rad]    4th col:  Real part [as Factor not dB!] 5th col: Imaginary part [as Factor not dB!] (so only first 3 columns are needed)
To get dB Value: Amplitude[dB] = 20 log [Magnitude]
Usually the Magnitude was calculated as response/reference (input) in the frequency domain. As for measuring the mechanical admittance the sensor is most likely an accelerometer (capturing the response in m/s2 of the object of interest) and the reference an impact hammer capturing the input force in Newton. As the mechanical admittance is defined as v/F (speed over force) the acceleration signal has to be integrated. The here captured signals are integrated in the frequency domain, what means the magnitude is divided by the corresponding frequency value in s-1. Values coded like: 3.30750000000000E+1 -> 3.3075 * 10 -> 33.075
DOI: 10.6084/m9.figshare.24523540
title: GC-MS data of essential oils of <i>Zanthoxylum armatum</i> DC. from different production areas

description: GC-MS data of essential oils of <i>Zanthoxylum armatum</i> DC. from different production areas
DOI: 10.6084/m9.figshare.24523540.v1
title: GC-MS data of essential oils of <i>Zanthoxylum armatum</i> DC. from different production areas

description: GC-MS data of essential oils of <i>Zanthoxylum armatum</i> DC. from different production areas
DOI: 10.5281/zenodo.10079910
title: Bridge admittance measurements of a Moroccan rabāb

description: Instrument: rabāb Country of origin: Morocco Place of origin: Fès Instrument maker: Abdessalam Chiki Year of manufacture: 2015 Location: Basel, private property of Thilo Hirsch
Dimensions: Total length: 513.2 mm Max. Body width: 114.8 mm Width at the upper end of the skin: 96.2 mm Width at top nut: 31.6 mm Body depth at the upper end of the skin: approx. 80 mm
Vibrating string lengths: d-string: 410 mm G-string: 403 mm
Materials: Body: walnut Pegbox: walnut Fingerboard: acajou (mahogany) Decoration: mother-of-pearl Bars: spruce Top nut, tailpiece button: bone Bridge: bamboo Top: goatskin
Bridge admittance measurements: Alexander Mayer, mdw - University of Music and Performing Arts Vienna, Department of Music Acoustics – Wiener Klangstil (IWK), 18.2.2020
Force: Impact hammer exciting at the bass side of the bridge.ACC: Acceleration measured on the same side.Average is the average of all measurements (to be used in the analysis).
Photos of the setup: Thilo Hirsch
________________________
How to read VIA-Files: Line 1 to 9: Header, Line 8 holds the number of values
Data is organized as followed: 1st col: Frequency [Hz]          2nd col: Magnitude [as Factor not dB!]        3rd col: Phase [rad]    4th col:  Real part [as Factor not dB!] 5th col: Imaginary part [as Factor not dB!] (so only first 3 columns are needed)
To get dB Value: Amplitude[dB] = 20 log [Magnitude]
Usually the Magnitude was calculated as response/reference (input) in the frequency domain. As for measuring the mechanical admittance the sensor is most likely an accelerometer (capturing the response in m/s2 of the object of interest) and the reference an impact hammer capturing the input force in Newton. As the mechanical admittance is defined as v/F (speed over force) the acceleration signal has to be integrated. The here captured signals are integrated in the frequency domain, what means the magnitude is divided by the corresponding frequency value in s-1. Values coded like: 3.30750000000000E+1 -> 3.3075 * 10 -> 33.075
DOI: 10.5281/zenodo.10079909
title: Bridge admittance measurements of a Moroccan rabāb

description: Instrument: rabāb Country of origin: Morocco Place of origin: Fès Instrument maker: Abdessalam Chiki Year of manufacture: 2015 Location: Basel, private property of Thilo Hirsch
Dimensions: Total length: 513.2 mm Max. Body width: 114.8 mm Width at the upper end of the skin: 96.2 mm Width at top nut: 31.6 mm Body depth at the upper end of the skin: approx. 80 mm
Vibrating string lengths: d-string: 410 mm G-string: 403 mm
Materials: Body: walnut Pegbox: walnut Fingerboard: acajou (mahogany) Decoration: mother-of-pearl Bars: spruce Top nut, tailpiece button: bone Bridge: bamboo Top: goatskin
Bridge admittance measurements: Alexander Mayer, mdw - University of Music and Performing Arts Vienna, Department of Music Acoustics – Wiener Klangstil (IWK), 18.2.2020
Force: Impact hammer exciting at the bass side of the bridge.ACC: Acceleration measured on the same side.Average is the average of all measurements (to be used in the analysis).
Photos of the setup: Thilo Hirsch
________________________
How to read VIA-Files: Line 1 to 9: Header, Line 8 holds the number of values
Data is organized as followed: 1st col: Frequency [Hz]          2nd col: Magnitude [as Factor not dB!]        3rd col: Phase [rad]    4th col:  Real part [as Factor not dB!] 5th col: Imaginary part [as Factor not dB!] (so only first 3 columns are needed)
To get dB Value: Amplitude[dB] = 20 log [Magnitude]
Usually the Magnitude was calculated as response/reference (input) in the frequency domain. As for measuring the mechanical admittance the sensor is most likely an accelerometer (capturing the response in m/s2 of the object of interest) and the reference an impact hammer capturing the input force in Newton. As the mechanical admittance is defined as v/F (speed over force) the acceleration signal has to be integrated. The here captured signals are integrated in the frequency domain, what means the magnitude is divided by the corresponding frequency value in s-1. Values coded like: 3.30750000000000E+1 -> 3.3075 * 10 -> 33.075
DOI: 10.34740/kaggle/dsv/6920189
title: Global Genomic Neurofibromatosis Neoplasia
DOI: 10.5281/zenodo.10079591
title: Laser interferometry measurements of a Moroccan rabāb

description: Instrument: rabāb Country of origin: Morocco Place of origin: Fès Instrument maker: Abdessalam Chiki Year of manufacture: 2015 Location: Basel, private property of Thilo Hirsch
Dimensions: Total length: 513.2 mm Max. Body width: 114.8 mm Width at the upper end of the skin: 96.2 mm Width at top nut: 31.6 mm Body depth at the upper end of the skin: approx. 80 mm
Vibrating string lengths: d-string: 410 mm G-string: 403 mm
Materials: Body: walnut Pegbox: walnut Fingerboard: Acajou (mahogany) Decoration: mother-of-pearl Bars: spruce Top nut, tailpiece button: Bone Bridge: bamboo Top: goatskin
Laser interferometry measurements: Alexander Mayer, mdw - University of Music and Performing Arts Vienna, Department of Music Acoustics – Wiener Klangstil (IWK), 18.2.2020
Each figure (Filenames: A_####Hz.jpg) corresponds to the frequency of excitation on the bass side of the bridge (shaker: Frederiksen Vibration Generator Nr 2185.00). Images are made by time-averaging of laser speckle interference at the camera (time-average ESPI approach). Operating deflection shapes (roughly translating to theoretical vibrating modes) are observed at each frequency.
Photo of the setup: Thilo Hirsch