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Zvaigžņotā Debess: 2010/11, Ziema (210)

2010

Contents: “ZVAIGŅOTĀ DEBESS” FORTY YEARS AGO: Bursting Stars. J. Francman (abridged). Geodesists Help Renew the Spire of St. Peter’s Church. J. Klētnieks (abridged). DEVELOPMENTS in SCIENCE: The Solar Neutrino Problem. O. Smirnova. NEWS: At Last the Planet at the Star β Pictoris Is Imaged. A. Alksnis, Z. Alksne. SPACE RESEARCH and EXPLORATION: The Trail of an Asteroid Reveals a Recent Collision. A. Alksnis. INTERNATIONAL YEAR of ASTRONOMY 2009: International Year of Astronomy 2009 in Philately. The Rest of the World except Series EUROPA (concluded). J. Limansky. ACADEMIC STAFF of the UNIVERSITY of LATVIA: Assistant Professor in Physics Ojārs Šmits (24.04.1930.-14.03.1993.) of the Latvian Un…

Baldones skolēni Maskavā un LisabonāStarptautiskie kosmiskie lidojumi – pastmarkasPubliskie saules pulksteņi LatvijāAlfonam Apinim – 100Vistālākā galaktikaEmanuels GrinbergsJupitera bombardēšana – amatieru novērojumiPlanētu redzamības kompleksā diagramma 2011J.Stradiņa monogrāfija „Zinātnes un augstskolu sākotne Latvijā”Astronomija filatēlijāSaules neitrīnoRainis Zvaigžņotā Debess un DainasNASA’s zonde Deep Impact un komēta Hartley 2Fricis GulbisAsteroīda P/2010 A2 astePilns Saules aptumsums - 2010.g. 11.jūlijs Francijas PolinēzijaGrāmata „Einšteins. Viņa dzīve un Visums”Astronomiskās parādības - 2010Astronomiskās parādības - 2011Par Nibiru un Pasaules galuLU fizikas docents Ojārs Šmits (1930-1993)Koncerts Astrophonia ValmierāLatvijas Astronomijas biedrības observatorija SiguldāPar misēkļiem Astronomiskajā kalendārā 2011V.Struves ģeodēziskais loks - pastmarkasValdemāram Murevskim – 100Zvaigznes Gleznotāja β planētaMstislavam Keldišam – 100Jaunākie ieguvumi “Zvaigžņotās Debess” bibliotēkāDaļējs Saules aptumsums 2011.gada 4.janvārīMarsa ekspedīciju kuģu Orion un Dragon maketiSkaitļu pieraksti senajās kultūrās
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Bitumen stabilized ballast: a potential solution for railway track-bed

2016

Railway ballast degradation under dynamic loads progressively leads to loss of mechanical performance and geometry of the track, so that maintenance interventions are frequently needed. In order to system- atically avoid this issue, recently solutions have been proposed to reinforce track-bed by using polyur- ethane and/or resins as well as asphalt layers among others. Nonetheless, their main limitations are related to the high initial cost and low productivity. To cope with these limitations, in this study, bitumen stabilized ballast (BSB) is proposed as a new solu- tion for ballast stabilization. This method aims at improving durability and reducing settlement by mod- ifying both stiffnes…

BallastEngineering0211 other engineering and technologiesCompaction02 engineering and technologyTrack (rail transport)021105 building & constructionBallast recyclingmedicineSettore ICAR/04 - Strade Ferrovie Ed AeroportiGeneral Materials ScienceGeotechnical engineering021101 geological & geomatics engineeringCivil and Structural EngineeringBitumen stabilized ballast Railway trackbed maintenance Ballast stabilization Ballast recyclingBallast stabilizationbusiness.industrySettlement (structural)StiffnessBuilding and ConstructionStructural engineeringDissipationDurabilityBitumen stabilized ballastAsphaltmedicine.symptombusinessRailway trackbed maintenance
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Novel performance-based technique for predicting maintenance strategy of bitumen stabilised ballast

2018

Abstract Despite being the most used worldwide, railway ballasted tracks presents high maintenance cost related to ballast settlement and particle degradation. With the aim of reducing life cycle costs, bitumen stabilised ballast (BSB) has been recently proposed as a relatively cheap alternative maintenance solution to be applied to existing tracks. This study aims at assessing the potential advantages of this technology, defining a novel maintenance strategy of traditional ballasted track-beds. A protocol for the application of the BSB technology and its associated maintenance strategy is defined. To estimate minor and major maintenance operations of BSB scenario in comparison to tradition…

BallastEngineeringMaintenance0211 other engineering and technologiesRailway ballastDegradation model020101 civil engineering02 engineering and technologyBitumen stabilisationTrack (rail transport)0201 civil engineeringTamping021105 building & constructionLife cycle costsSettore ICAR/04 - Strade Ferrovie Ed AeroportiGeneral Materials ScienceSensitivity (control systems)Civil and Structural EngineeringSettlementbusiness.industrySettlement (structural)Maintenance strategyBuilding and ConstructionReliability engineeringBitumen stabilisation; Degradation model; Life cycle approach; Maintenance; Railway ballast; Settlement; Tamping; Civil and Structural Engineering; Building and Construction; Materials Science (all)AsphaltMaterials Science (all)businessLife cycle approachMarine engineeringConstruction and Building Materials
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Use of bitumen-stabilised ballast for improving railway trackbed conventional maintenance

2018

Despite its many advantages, ballasted track needs frequent maintenance to ensure an adequate quality of service. However, tamping, traditionally used to correct geometry, causes ballast degradation and loosening of the already compacted ballast layer, which quickly returns the track to its pre-maintenance position. Then, other maintenance techniques such as stoneblowing, as well as diverse solutions that reinforce trackbed, have been developed to reduce ballast settlement and particles degradation. Given the need to further advance research in this field, bitumen-stabilised ballast (BSB) has started to be investigated by the authors as a feasible solution thanks to its easy and quick appl…

BallastSettlementEngineeringbusiness.industryLaboratory tests0211 other engineering and technologies02 engineering and technologyGeotechnical Engineering and Engineering GeologyTrack (rail transport)StiffnessFull-scale testsAsphalt021105 building & constructionEarth and Planetary Sciences (miscellaneous)Forensic engineeringFull scale testSoil stabilisationbusiness021101 geological & geomatics engineeringGéotechnique
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Effects of forest restoration treatments on the abundance of bark beetles in Norway spruce forests of southern Finland

2009

Abstract Restoration of protected areas in boreal forests frequently includes creating substantial volumes of dead wood. While this benefits a wide range of dead wood dependent invertebrate species, some of these are regarded as forest pests. Therefore, the risk of elevated levels of tree mortality in surrounding commercial forests must be considered. In a large-scale field experiment in southern Finland, we studied the effects of restoration treatments on the abundance of bark beetles within and in the vicinity of restored areas, in particular focusing on Ips typographus and Pityogenes chalcographus . The treatments applied to managed Norway spruce forests were controlled burning and parti…

Bark beetlebiologyEcologyTaigaForestryPicea abiesManagement Monitoring Policy and Lawbiology.organism_classificationcomplex mixturesForest restorationvisual_artCurculionidaevisual_art.visual_art_mediumBarkRestoration ecologyNature and Landscape ConservationWoody plantForest Ecology and Management
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Petrogenetic evolution of metabasalts and metakomatiites of the lower Onverwacht Group, Barberton Greenstone Belt (South Africa)

2019

A well-preserved sequence, by Archean standards, of mantle-derived metabasalts and metakomatiites forms large parts of the lower Onverwacht Group of the Barberton Greenstone Belt (South Africa). To elucidate the origin of mafic and ultramafic rocks from this 3.55 to 3.45 Ga sequence, we present a comprehensive geochemical dataset including major and trace elements as well as Lu-Hf and Sm-Nd isotope compositions for a variety of metavolcanic rocks. These include metabasalts of the amphibolite-facies Sandspruit and Theespruit Formations as well as metabasalts and metakomatiites of the lower greenschist-facies Komati Formation. Based on their incompatible trace element patterns, the basalts of…

Basalt010504 meteorology & atmospheric sciencesArcheanPartial meltingTrace elementGeochemistryGeologyGreenstone belt010502 geochemistry & geophysics01 natural sciencesMantle plumeGeochemistry and PetrologyUltramafic rockddc:550Institut für GeowissenschaftenPrimitive mantleGeology0105 earth and related environmental sciences
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The Late Cretaceous Klepa basalts in Macedonia (FYROM) – Constraints on the final stage of Tethys closure in the Balkans

2017

The waning stage(s) of the Tethyan ocean(s) in the Balkans are not well understood. Controversy centres on the origin and life-span of the Cretaceous Sava Zone, which is allegedly a remnant of the last oceanic domain in the Balkan Peninsula, defining the youngest suture between Eurasia- and Adria-derived plates. In order to investigate to what extent late-Cretaceous volcanism within the Sava zone is consistent with this model, we present new age data together with trace-element and Sr–Nd–Pb isotope data for the Klepa basaltic lavas from the central Balkan Peninsula. Our new geochemical data show marked differences between the Cretaceous Klepa basalts (Sava Zone) and the rocks of other volca…

Basalt010504 meteorology & atmospheric sciencesSubductionPolybaric meltingGeology010502 geochemistry & geophysicsOphiolite01 natural sciencesMantle (geology)CretaceousPaleontology13. Climate actionMagmatism14. Life underwaterForearcGeology0105 earth and related environmental sciences
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Geochemical constraints on basalt petrogenesis in the Strait of Sicily Rift Zone (Italy): Insights into the importance of short lengthscale mantle he…

2020

Igneous activity from the late Miocene to historic time (most recently 1891 CE) in the Strait of Sicily has created two volcanic islands (Pantelleria and Linosa) and several seamounts. These volcanoes are dominated by transitional (ol + hy-normative) to alkaline (ne-normative) basaltic lavas and scoriae; volcanic felsic rocks (peralkaline trachyte-rhyolite) crop out only on Pantelleria. Although most likely erupted through continental crust, basalts demonstrate no evidence of crustal contamination and are geochemically similar to oceanic island basalts (OIB). Despite their isotopic similarities, there are considerable compositional differences with respect to major and trace element geochem…

BasaltContinental-OIBStrait of Sicily Rift ZoneFelsicAlkali Basalt010504 meteorology & atmospheric sciencesContinental crustAlkali basaltKeywords: Strait of Sicily Rift Zone Continental-OIB Alkali basalt Mantle melting Mantle heterogeneitySettore GEO/07 - Petrologia E PetrografiaPartial meltingGeochemistryGeologyCrust010502 geochemistry & geophysics01 natural sciencesMantle (geology)Geochemistry and PetrologyAsthenosphereMantle HeterogeneityMantle MeltingGeology0105 earth and related environmental sciencesChemical Geology
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Metamorphism and melting of picritic crust in the early Earth

2014

Abstract Partial melting experiments with models of Archean oceanic crust (MAOC; with 11, 13 and 15 wt.% MgO) are used to investigate the role of metamorphism and melting of primary picritic compositions in the formation of TTG-like melts and continental crust on the early Earth. The approach investigates the possibility that the average early crust composition was comparatively MgO-rich and evolved to lower magnesium content during the secular cooling of the Earth. High-pressure partial melting experiments indicate a transition of melt compositions from aluminous basaltic melts in MAOC 15 to predominantly tonalitic melts in MAOC 11 and higher melting temperatures with increasing magnesium …

BasaltGeochemistry and PetrologyOceanic crustContinental crustAdakiteGeochemistryPartial meltingGeologyCrustGranuliteMantle (geology)GeologyLithos
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Petrology of mafic lavas within the Onega plateau, central Karelia: evidence for 2.0 Ga plume-related continental crustal growth in the Baltic Shield

1998

The Onega plateau constitutes part of a vast continental flood basalt province in the SE Baltic Shield. It consists of Jatulian-Ludikovian submarine volcanic, volcaniclastic and sedimentary sequences attaining in places 4.5 km in thickness. The parental magmas of the lavas contained ∼10% MgO and were derived from melts generated in the garnet stability field at depths 80–100 km. The Sm-Nd mineral and Pb-Pb whole-rock isochron ages of 1975 ± 24 and 1980 ± 57 Ma for the upper part of the plateau and a SHRIMP U-Pb zircon age of 1976 ± 9 Ma for its lower part imply the formation of the entire sequence within a short time span. These ages coincide with those of picrites in the Pechenga-Imandra b…

BasaltGeophysicsGeochemistry and PetrologyContinental crustFlood basaltGeochemistryBaltic ShieldOcean island basaltMaficPetrologyGeologyMantle plumeZirconContributions to Mineralogy and Petrology
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