Relevant bibliographies by topics / Timavo

Academic literature on the topic 'Timavo'

Author: Grafiati
Published: 11 March 2023

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Journal articles on the topic "Timavo"

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Gabrovšek, Franci, Andrej Mihevc, Cyril Mayaud, Matej Blatnik, and Blaž Kogovšek. "Slovene Classical karst: Kras Plateau and the Recharge Area of Ljubljanica River / Klasični kras: planota Kras in kraško zaledje izvirov Ljubljanice." Folia biologica et geologica 63, no. 2 (September 7, 2022): 35–60. http://dx.doi.org/10.3986/fbg0097.

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The area of the Classical Karst is roughly defined by a triangle with Ljubljana, Trieste and Rijeka as its vertices. This is the area where the first scientific studies of karst phenomena were conducted. Two sub-regions that particularly attracted researchers are presented. Kras/Carso plateau with the Škocjan caves and the underground course of the Reka river. The groundwater flow of Reka-Timavo is characterised by high recharge variability of allogenic inflow of Reka River and flow restrictions in the upper part of subterranean flow, which control regional backfloodings observed in cave systems. The recharge area of Ljubljanica Springs is known for a cascading series of poljes in intermediate cave systems. The area has been in focus of hydrological studies for over a century, but many phenomena have been resolved in the last decade based on results of continuous autonomous monitoring in the last decade. Key words: Classical Karst, Kras, Škocjanske Jame, Reka-Timavo system, Ljubljanica Recharge Area, Polje. IZVLEČEK Območje Klasičnega krasa v grobem objema trikotnik z Ljubljano, Reko in Trstom v ogliščih. Tu se je začelo znanstveno proučevanje krasa. Dve kraški območji sta tu še posebej pritegnili pozornost raziskovalcev. Prvo je planota Kras s Škocjanskimi jamami in podzemnim tokom Reke med Škocjanskimi jamami in izviri Timave. Ta tok močno zaznamuje velika spremenljivost dotoka reke Reke in lokalne zožitve v vodonosniku, ki povzročajo regionalno poplavljanje, kot ga beležimo v jamah. Drugo je območje kraške Ljubljanice z značilnim nizom dinarskih kraških polj in jamskih sistemov, ki polja hidrološko povezujejo. Območje je že več kot stoletje predmet številnih raziskav, zvezno spremljanje parametrov toka v kraških jamah v zadnjih desetih letih, pa je omogočilo nova spoznanja o lastnostih in mehanizmih pretakanja vode v celotnem sistemu. Ključne besede: Klasični kras, Kras, Škocjanske jame, podzemni tok reke Reke, kraško zaledje izvirov Ljubljanice, polje.
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Forti, Fabio. "La storia della Speleologia Triestina in relazione al problema Timavo." International Journal of Speleology 18, no. 1/2 (January 1989): 65–72. http://dx.doi.org/10.5038/1827-806x.18.1.4.

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Giani, Michele, Nives Ogrinc, Samo Tamše, and Stefano Cozzi. "Elevated River Inputs of the Total Alkalinity and Dissolved Inorganic Carbon in the Northern Adriatic Sea." Water 15, no. 5 (February 25, 2023): 894. http://dx.doi.org/10.3390/w15050894.

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The response of coastal systems to global acidification depends strongly on river inputs, which can alter the total alkalinity (AT) and dissolved inorganic carbon (DIC) in seawater. The northern Adriatic Sea (NAd) is a shallow continental shelf region that currently receives about 15% of the total freshwater input in the Mediterranean Sea, where the role of riverine discharges on the carbonate system has been poorly studied. In particular, river discharges can alter the carbonate system in the sea, affecting both the equilibrium chemistry and biological processes. For the main rivers flowing into the NAd (the Po, Adige, Brenta, Piave, Livenza, Tagliamento, Isonzo, Timavo and Rižana), data were collected for the pH, concentrations of the total alkalinity (AT), Ca2+ and Mg2+ and the isotopic ratio of stable carbon in the dissolved inorganic carbon (δ13CDIC). The DIC fluxes were estimated using the THINCARB (THermodynamic modeling of INOrganic CARBon) model for the compilation of the AT and pH data. The results show that the total transport of the AT in the rivers was 205 Gmol yr−1 while the transport of the DIC was 213 Gmol yr−1, of which about 70% was from the Po River. About 97% of the DIC in the river waters was in the form of bicarbonates. The high Mg2+/Ca2+ ratios indicate that dolomite weathering is predominant in the Adige, Piave, and Livenza river basins, while lower ratios in the Timavo and Rižana rivers indicate a greater proportion of calcite. The mean δ13C-DIC value was estimated to be −10.0 ± 1.7 ‰, a value nowadays considered typical for the DIC flux inputs in oceanic carbon cycle modeling. The DIC flux depends on the mineral weathering and biological activity in each river basin. However, these natural processes can be modified by anthropogenic disturbances that should be better quantified.
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Reisenhofer, E., G. Adami, and P. Barbieri. "Using chemical and physical parameters to define the quality of karstic freshwaters (Timavo River, North-eastern Italy): a chemometric approach." Water Research 32, no. 4 (April 1998): 1193–203. http://dx.doi.org/10.1016/s0043-1354(97)00325-4.

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Calligaris, Chiara, Kim Mezga, Francesca Slejko, Janko Urbanc, and Luca Zini. "Groundwater Characterization by Means of Conservative (δ18O and δ2H) and Non-Conservative (87Sr/86Sr) Isotopic Values: The Classical Karst Region Aquifer Case (Italy–Slovenia)." Geosciences 8, no. 9 (August 28, 2018): 321. http://dx.doi.org/10.3390/geosciences8090321.

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The study of the different hydrogeological compartments is a prerequisite for understanding and monitoring different fluxes, thereby evaluating the environmental changes in an ecosystem where anthropogenic disturbances are present in order to preserve the most vulnerable groundwaters from contamination and degradation. In many karst domains in the Mediterranean, areas groundwaters and surface waters are a single system, as a result of the features that facilitate the ingression of waters from surface to subsurface. This is also the case for the Classical Karst hydrostructure, which is a carbonate plateau that rises above the northern Adriatic Sea, shared between Italy and Slovenia. The main suppliers to the aquifer are the effective precipitations and the waters from three different rivers: Reka/Timavo, Soča/Isonzo and Vipava/Vipacco. Past and ongoing hydrogeological studies on the area have focused on the connections within the Classical Karst Region aquifer system through the analysis of water caves and springs hydrographs and chemographs. In this paper, the authors present new combined data from major ions, oxygen, hydrogen and strontium stable and radiogenic isotopes which have allowed a more complementary knowledge of the groundwater circulation, provenance and water-rock interactions. All the actions occurred in the framework of the European project HYDROKARST.
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Luštrik, Roman, Martin Turjak, Simona Kralj-Fišer, and Cene Fišer. "Coexistence of surface and cave amphipods in an ecotone environment." Contributions to Zoology 80, no. 2 (April 14, 2011): 133–41. http://dx.doi.org/10.1163/18759866-08002003.

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Interspecific interactions between surface and subterranean species may be a key determinant for species distributions. Until now, the existence of competition (including predation) between these groups has not been tested. To assess the coexistence and potential role of interspecific interactions between surface Gammarus fossarum and subterranean Niphargus timavi, and to determine their micro distributions, we conducted a series of field and laboratory observations. We aimed to determine: (1) species substrate preference, (2) whether the presence of G. fossarum influences the habitat choice of N. timavi, and (3) possible predation effects on micro habitat choice of small juveniles. Throughout a small river in SW Slovenia, N. timavi was predominantly found in leaf litter and gravel, but rarely in sand. In the sand however, we exclusively found juveniles. In contrast, surface G. fossarum sheltered mainly in leaf litter. A similar, body size dependent, micro distribution was observed in G. fossarum, where small individuals were generally found in gravel and sand. The presence of G. fossarum affected the micro distribution of juvenile, but not adult, N. timavi. In the laboratory we observed predation and cannibalism in both species. Niphargus timavi, however, appeared to be a more efficient predator than G. fossarum. In particular, juvenile N. timavi were most vulnerable to preying by adults of both species. This probably affected the distribution of juvenile N. timavi that chose finer substrates when placed with adult individuals in an aquarium with granules of different size. To understand the distribution of subterranean species, the summed effect of intraspecific interactions, as well as surface – subterranean species interactions, in particular between individuals of different size, should be taken into account.
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Sari, Intan. "Analisis pendapatan usaha kopi tubruk Gayo di Desa Conto Kecamatan Timang Gajah Kabupaten Bener Meriah." Jurnal Sains Pertanian (JSP) 6, no. 3 (October 31, 2022): 114–19. http://dx.doi.org/10.51179/jsp.v6i3.1751.

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Penelitian ini dilakukan pada Usaha Kopi Tubruk Gayo di Desa Conto Kecamatan Timang Gajah Kabupaten Bener Meriah. Tujuan penelitian untuk mengetahui pendapatan Usaha Kopi Tubruk Gayo di Desa Conto Kecamatan Timang Gajah Kabupaten Bener Meriah dan menganalisis Kelayakan Usaha Kopi Tubruk Gayo di Desa Conto Kecamatan Timang Gajah Kabupaten Bener Meriah. Berdasarkan hasil penelitian pada usaha Bubuk Kopi Tubruk Gayo di Desa Conto Kecamatan Timang Gajah Kabupaten Bener Meriah diperoleh bahwa rata-rata penerimaan pada usaha produksi Bubuk Kopi Tubruk Gayo di Desa Conto Kecamatan Timang Gajah Kabupaten Bener Meriah adalah Rp. 450.000.000,00/tahun. Sementara keuntungan yang diperoleh sebesar Rp. 329.853.750/tahun. Perhitungan B/C rasio adalah 2,75, atau 2,75 > 0, Hal ini menunjukkan bahwa usaha produksi Bubuk Kopi Tubruk Gayo di Desa Conto Kecamatan Timang Gajah Kabupaten Bener Meriah dapat dikatakan menguntungkan dan layak dijalankan. Kata kunci : Analisis, Pendapatan, Kopi Tubruk
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Fatimah, Fatimah. "RESEPSI MASYARAKAT DAN NILAI PENDIDIKAN KARAKTER CERITA DATU TIMANG (COMMUNITY RECEPTION AND THE VALUE OF CHARACTER EDUCATION IN THE LEGEND OF DATU TIMANG)." JURNAL BAHASA, SASTRA DAN PEMBELAJARANNYA 12, no. 1 (March 30, 2022): 161. http://dx.doi.org/10.20527/jbsp.v12i1.13052.

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AbstractCommunity Reception and the Value of Character Education in the Legend of DatuTimang. This study aims to describe the factors causing reception actions / forms ofcommunity receptions, and the value of character education in the Datu Timang story.This research is a descriptive qualitative research through a literary reception approach.Sources of research data were taken from the informants' speech either throughinterviews, field observations at Datu Timang's grave, and manakib documents or booksrelated to Datu Timang. The results of this study are (1) it can be seen the forms ofcommunity reception of Datu Timang's story in the form of a biography. Theimplementation of the Datu Timang haul, the number of pilgrims to the grave of DatuTimang, the habit of reading manakib, the presence of people who are fluent in telling thehistory of Datu Timang, and the document manakib / books that were published. Thefactors influensing are the the factors of the existence of vows, factors of love forguardians, actors whisful thinking/desires (marriage fartners,offspring/children,sustenance,etc.), socio-cutural factors, meanwhile. (2) it can be seen thevalue of character education in the story so that it can be an example for readers,especially the younger generation, namely. (1) religious (faith, piety, and gratitude); (2)responsibility; (3) social care (prioritizing public interests, being helpful, willing tosacrifice, cooperating, sharing, and loving; (4) discipline; (5) humble; (6) courageous;(7) hard work.Key words: community reception, legendary stories, Datu Timang, value, character educationAbstrakResepsi Masyarakat dan Nilai Pendidikan Karakter Cerita Datu Timang. Penelitianini bertujuan untuk mendeskripsikan bentuk-bentuk resepsi masyarakat dan nilaipendidikan karakter yang ada dalam cerita Datu Timang. Penelitian ini berjenis penelitiankualitatif deskriptif melalui pendekatan resepsi sastra. Sumber data penelitian diambil darituturan informan baik melalui kegiatan wawancara mendalam, observasi lapangan dimakam Datu Timang, dan dokumen manakib atau buku yang berkaitan dengan DatuTimang. Hasil dari penelitian ini adalah (1) dapat diketahui bentuk-bentuk resepsimasyarakat terhadap cerita Datu Timang berupa riwayat hidup. pelaksanaan haul DatuTimang, banyaknya peziarah ke makam Datu Timang, adanya kebiasaan membacamanakib, adanya orang yang fasih menceritakan riwayat Datu Timang, dan adanyadokumen riwayat DT /manakib, atau buku cerita rakyat DT yang diterbitkan. Selain itujuga faktor-faktor yang mempengaruhinya adalah adanya nazar, faktor kecintaan terhadapwali, adanya angan-angan atau keinginan (jodoh,keturunan,rezeki,dsb.), faktor sosialbudaya, (2) dapat diketahui nilai pendidikan karakter yang ada pada cerita sehingga dapatmenjadi contoh bagi pembaca khususnya generasi muda, yaitu. (1) religius (iman, takwa,dan syukur); (2) tanggung jawab; (3) peduli sosial (mementingkan kepentingan umum,penolong, rela berkorban, kerja sama, suka berbagi, dan pengasih; (4) disiplin; (5) rendahhati; (6) pemberani; (7) kerja keras.Kata-kata kunci: resepsi masyarakat, cerita legenda, Datu Timang, nilai, pendidikan karakter
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Hershbell, Jackson. "Timaios of Loeri." Ancient Philosophy 5, no. 1 (1985): 126–27. http://dx.doi.org/10.5840/ancientphil19855140.

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Cameselle, R., J. Oliver, C. Martinez Vazquez, S. Pombo, B. Villoch, J. Quintana, and A. Pena. "Quiste timico mediastinico." Archivos de Bronconeumología 21, no. 3 (May 1985): 140–41. http://dx.doi.org/10.1016/s0300-2896(15)32188-8.

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Dissertations / Theses on the topic "Timavo"

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Falconi, Claus Francois. "Complex water column nutrient dynamics in the Gulf of Trieste; freshwater nutrient discharge Vs biologicallly mediated cycling of dissolved organic matter." Doctoral thesis, Università degli studi di Trieste, 2009. http://hdl.handle.net/10077/3172.

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2007/2008
Il Golfo di Trieste, localizzato nella parte più settentrionale ed orientale del bacino Adriatico, rappresenta un’area peculiare per le sue caratteristiche geomorfologiche, oceanografiche e biologiche. In quest’area, in particolare, insistono diverse attività economiche che vanno dalla maricoltura al turismo e pertanto i problemi legati alla qualità ambientale sono oltremodo diversificati: da un lato è importante che la trofia del sistema supporti lo sviluppo e la crescita dei molluschi allevati e dall’altro la fruizione delle acque per la balneazione richiede requisiti di qualità precisi e stabiliti dalle normative europee. Alla base di qualsiasi approccio gestionale all’ambiente marino costiero è comunque necessario conoscere la dinamica dei composti che stanno alla base della rete alimentare e che rappresentano anche importanti segnali di apporti antropici al sistema. I nutrienti, siano essi nella forma inorganica o in quella organica, regolano le dinamiche trofiche dell’ecosistema costiero e sono oltremodo concentrati in prossimità di scarichi urbani o nelle acque a bassa salinità frutto del mescolamento tra fiume e mare. Nonostante i numerosi e approfonditi studi sull’ecosistema del Golfo di Trieste, la dinamica dei nutrienti è stata poco approfondita, soprattutto in relazione alla frazione organica. La ricerca svolta nell’ambito di questo dottorato ha avuto come obiettivi principali: La valutazione delle dinamiche spaziali e temporali della concentrazione dei macronutrienti, nella forma inorganica ed organica, nelle acque del Golfo di Trieste La verifica del ruolo degli apporti fluviali e antropici sulla loro disponibilità La comprensione dell'importanza delle attività microbiche di rimineralizzazione sulla disponibilità degli stessi. Il protocollo sperimentale ha previsto l'analisi di campioni d'acqua prelevati mensilmente in 9 stazioni del Golfo, nel periodo 2004-2008. Nella stazione storica C1 il campionamento è stato intensificato per meglio valutare le dinamiche temporali esplorando la variabilità giornaliera e quella a scala oraria. Poiché il Golfo è soggetto a notevoli apporti fluviali, è stato valutato il ruolo dell’Isonzo, il fiume più importante, e, a partire dal 2006, è stato considerato anche il Timavo. Per evidenziare il ruolo degli scarichi antropici sono stati considerati i dati provenienti dal Monitoraggio delle acque costiere predisposto dalla Regione FVG (2002-2005). L’imponente lavoro analitico ha permesso di confermare la scarsa disponibilità di fosforo nelle acque del Golfo anche in periodi di limitata utilizzazione biologica. L’apporto dei fiumi arricchisce le acque delle forme particellate ma non incide sulla frazione disciolta mentre gli scarichi urbani non influenzano significativamente la disponibilità. Importante risulta, invece, il ruolo della degradazione enzimatica della sostanza organica. Sia il fitoplancton che il batterioplancton producono, infatti, notevoli quantità di fosfatasi alcalina, enzima in grado di recuperare fosforo da molecole organiche. Attraverso la produzione di enzimi, i microrganismi riescono a sopperire alla scarsa disponibilità di molecole inorganiche, più facilmente utilizzabili ma estremamente meno abbondanti. Questi risultati sono oltremodo importanti per l’organizzazione dei futuri piani di monitoraggio degli ambienti marini costieri caratterizzati da forti input di acqua dolce sia di origine antropica che fluviale. La trofia del sistema, infatti, non è sostenuta soltanto dai Sali inorganici disciolti di azoto, fosforo e silicio ma è fortemente dipendente dal pool di organico sia disciolto che particellato. L’attività degradativi dei microrganismi su queste matrici consente loro di ottenere le sotanze essenziali per la crescita e la duplicazione.
XIX Ciclo
1966
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Grillo, Barbara. "Ricostruzione dell’idrodinamica delle acque di falda del Carso Classico." Doctoral thesis, Università degli studi di Trieste, 2013. http://hdl.handle.net/10077/8665.

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2011/2012
All'interno del massiccio carsico del Carso Classico si sviluppa il reticolo del cosiddetto Timavo ipogeo, uno tra i più famosi fiumi carsici al mondo, il cui percorso stimato in circa 80 km di sviluppo lineare tra Slovenia e Italia, nonostante sia stato oggetto di oltre due secoli di studi scientifici, è per alcuni aspetti misterioso. L’obiettivo di questa Tesi è: 1)la riorganizzazione e ottimizzazione della rete di monitoraggio delle acque di falda del Carso Classico; 2)l’analisi dei dati in continuo esistenti (portate, precipitazioni, livello, temperatura e conducibilità); 3)l’analisi dell’influenza del carico idraulico sull’idrostruttura; 4) la ricostruzione dell’idrodinamica nelle diverse condizioni di impinguamento per una valutazione della vulnerabilità e dell’entità delle risorse. L’attività di ricerca si è articolata essenzialmente in una prima fase di ricerca bibliografica e acquisizione delle competenze di gestione della rete di monitoraggio; una seconda parte di acquisizione delle competenza informatiche per l’analisi dei dati; una terza parte di interpretazione dei dati e costruzione di un nuovo modello idrodinamico considerando i parametri chimico-fisici degli eventi di piena principali. Il punto di forza del presente studio è la riorganizzazione, l’aggiornamento e l’analisi congiunta di tutta la serie temporale a disposizione permettendo di ottenere un robusto modello idrodinamico dell’area in esame. Infatti sono stati considerati quasi 4000000 di dati complessivi raccolti a cadenza oraria o bioraria in 17 anni: essi consistono in misure di livello, temperatura, conducibilità e torbidità delle acque di 29 punti di misura in 13 cavità, 4 piezometri, 7 sorgenti, 2 laghi, 4 fiumi. Inoltre sono stati considerati anche dati idrometrici, pluviometrici, di portata e dati geofisici di stazioni geodetiche. L’intervallo temporale analizzato va dal 1995 al 2012. La ricerca svolta costituisce un contributo allo studio secolare della complessa idrostruttura del Carso Classico e ha permesso di approfondire le conoscenze sulla sua idrodinamica. Si sono potuti evidenziare e caratterizzare i diversi comportamenti della circolazione idrica nei grandi condotti e nel reticolo fessurato, rilevando i settori a diversa idrodinamica e gettando le basi per una dettagliata mappatura di vulnerabilità e gestione della risorsa idrica. Sono stati raggiunti i seguenti obiettivi: 1)Realizzazione di una rete di monitoraggio integrata tra Italia e Slovenia per il monitoraggio qualitativo e quantitativo della falda del Carso classico; 2)Creazione di un ricco archivio dei dati idrologici (precipitazioni, temperature, portate, livelli, torbidità, conducibilità e temperature) dal 1995 ad oggi quale base fondamentale per la creazione di un sistema di gestione del territorio; 3)Aggiornamento della mappa delle precipitazioni del Carso Classico, unificando i dati italiani e sloveni e tenendo conto del quadro generale dato dall’OSMER e ARSO; 4)Analisi statistica comparata di tutti i dati acquisiti per caratterizzare ogni sito monitorato dal punto di vista chimico - fisico; 5)Analisi idrodinamica con l’elaborazione di un protocollo per il confronto del calcolo delle velocità apparenti da dati di temperatura e di conducibilità, grazie al quale poi è stato possibile calcolare le velocità apparenti su 17 eventi a regime diverso, validando la procedura mediante l’uso di tracciamenti storici; 6)Creazione di mappe isofreatiche in regime di magra e di piena del Carso Classico e della fascia delle sorgenti per la valutazione della distribuzione del carico idraulico; 7)Analisi quantitativa del livello, della temperatura e conducibilità di serie temporali mediante l’applicazione di funzioni matematiche (cross-correlazione e periodogramma) per testare e validare alcuni algoritmi; 8)Analisi multidisciplinare con la quale sono stati messi a confronto il segnale clinometrico dei pendoli in Grotta Gigante, il segnale GPS, i livelli della falda nell’Abisso di Trebiciano, nella Grotta Gigante e nel piezometro di Opicina per valutare l’influenza del carico idraulico.
XXV Ciclo
1977
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Pereira, Luiz Guilherme Couto. "Contra Timarco de Ésquines: tradução e estudo introdutório." Universidade de São Paulo, 2016. http://www.teses.usp.br/teses/disponiveis/8/8143/tde-20072016-190143/.

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Tradução e estudo do discurso \"Contra Timarco\", de Ésquines. O estudo se concentra na condição tríplice do texto, como discurso jurídico, retrato do comportamento sexual masculino da Atenas do Período Clássico e exemplo da recepção primitiva da obra homérica em uma situação distante do contexto dos festivais e simpósios.
Translation and study of the speech \"Against Timarchos\", by Aeschines. The analysis focus on the trifold condition of the text, as a juridical speech, a portrait of the male sexual behavior in Classic Athens and an example of early reception of Homer\'s poetry, in a condition that differs from festivals and symposiums.
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Lee, Kyung Jik. "Platons Raumbegriff : Studien zur Metaphysik und Naturphilosophie im "Timaios" /." [S.l. : s.n.], 1999. http://www.bsz-bw.de/cgi-bin/xvms.cgi?SWB8397801.

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Nikolaou, Sousanna-Maria. "Die Atomlehre Demokrits und Platons "Timaios" : eine vergleichende Untersuchungc /." Stuttgart : B. G. Teubner, 1998. http://catalogue.bnf.fr/ark:/12148/cb37552277v.

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Montenegro, Bernales Juan Ignacio. "Caracterización histológica del timo en fetos de alpaca." Bachelor's thesis, Universidad Nacional Mayor de San Marcos, 2006. https://hdl.handle.net/20.500.12672/668.

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El objetivo del presente trabajo fue el estudio citoarquitectural de los segmentos cervicales y torácicos del timo en fetos de alpaca (Lama pacos), que ofrece complementos al conocimiento de este órgano. Para tal propósito, se recolectaron 10 fetos entre 41 y 188 días de edad, y ellos fueron diseccionados y sometidos a estudio histológico. Los resultados más importantes muestran que el esbozo del timo a los 40 días tiene una morfología citoarquitectural de tipo acinar infiltrado por escasas células linfocíticas y rodeado por células mesenquimales. A los 60 días el esbozo del segmento cervical se presenta como un “folículo” linfoide densamente poblado por timocitos; mientras que la región torácica tiene una apariencia cavitaria con proyecciones trabeculares cortas hacia la zona interna del esbozo. La diferenciación de corteza y médula primero se evidencian en los segmentos cervicales posteriores y torácicos a los 100 días, donde el parénquima tímico comienza a tener proyecciones trabeculares más definidas, dándole la apariencia de seudolobulaciones y es a los 130 días donde se evidencia una tenue diferenciación entre corteza y médula en los segmentos cervicales anteriores. A los 165 días todos los segmentos cervicales, así como el torácico, presentan disposición lobulillar bien definidos en corteza y médula. La cápsula tímica se mantiene principalmente como una doble capa celular y tejido conjuntivo laxo. Los vasos sanguíneos subcapsulares y trabeculares presentan endotelio fenestrado. Las células eritroblásticas se ubican en las zonas subcapsulares y corticales periféricas desde los 100 días. La barrera hematotímica comienza a organizarse desde los 60 días. Los corpúsculos medulares de Hassal son evidentes a los 100 días, así como la barrera celular reticular epitelial en la zona corticomedular desde los 130 días. Palabras Clave: Alpaca, feto, timo, timocito, corpúsculo de Hassal.
--- The aim of the present research was to study the cellular architectural features of the thymus´ cervical and thoracic segments in alpaca fetuses (Lama pacos), and provide accurate information to the knowledge of this organ. For such purpose, 10 alpaca fetuses aged 41-188 days were collected, dissected and histologically analyzed. The most important results shown that the thymus´ anlage, at 40 days of age, had an acinar architectural morphology infiltrated by a few lymphoid cells and surrounded by mesenchymal cells. At 60 days of age, the anlage of cervical region appeared as a lymphoid “follicle” with a dense population of thymocites, whereas the thoracic region had a cystic appearance with short trabecular projections toward the anlage´s inner zone. At 100 days of fetal age, first differentiation between cortex and medulla was evident in the posterior cervical and thoracic segments, where the thymic parenchyma started to have well-defined trabecular projections, giving it an appearance of pseudolobullations. Also, at 130 days of age a little differentiation between the cortex and medulla in the anterior cervical segments was observed. At 165 days of fetal age, all the cervical and thoracical segments shown a well-defined lobular arrangement in the cortex and medulla. Thymic cap remained mainly as a double cellular layer of lax connective tissue. Subcapsular and trabecular blood vessels shown fenestrated endothelium. Erythroblastic cells in the peripheral subcapsular and cortical zones since 100 days were observed. Hema-thymic barrier started to be arranged since 60 days. Hassal´s medullar corpuscle at 100 days, as well as the epithelial reticular cellular barrier in the cortical-medullar zone since 130 days were seen. Key Words: Alpaca, fetus, thymus, thymocite, Hassal´s corpuscle.
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Gameiro, Jacy. "Aterações no microambiente timico frente a diferentes agentes indutores de atrofia." [s.n.], 2009. http://repositorio.unicamp.br/jspui/handle/REPOSIP/316964.

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Orientadores: Liana Verinaud, Wilson Savino
Tese (doutorado) - Universidade Estadual de Campinas, Instituto de Biologia
Made available in DSpace on 2018-08-13T05:50:49Z (GMT). No. of bitstreams: 1 Gameiro_Jacy_D.pdf: 7674475 bytes, checksum: 85104c8f2befe30630bf49436c0fb352 (MD5) Previous issue date: 2009
Resumo: O timo é o órgão linfóide primário responsável pelo amadurecimento dos linfócitos T. O processo de maturação é dependente da integridade do microambiente e da migração coordenada por elementos de matriz e quimiocinas dos precursores hematopoiéticos nos distintos nichos tímicos. Entretanto, a literatura mostra que profundas alterações no microambiente tímico, e conseqüentemente no desenvolvimento e amadurecimento dos linfócitos T, podem ocorrer como resultado de algumas patologias. No presente trabalho, analisamos a indução de atrofia e as alterações no microambiente tímico frente a três diferentes agentes indutores de atrofia, sendo dois agentes patogênicos, P.brasiliensis e P.berghei e uma doença metabólica, a diabetes induzida por aloxana. Nos três modelos estudados foi observada a atrofia do órgão com diferente intensidade nas alterações de componentes do microambiente tímico. Importantes moléculas associadas com a migração intratímica mostraram-se alteradas com modificações significativas nos elementos de matriz e nas quimiocinas bem como na expressão dos seus respectivos receptores. Ainda, a migração ex vivo também se mostrou alterada na atrofia induzida pelos agentes patogênicos, mas não no modelo de atrofia induzido por aloxana, sugerindo que as alterações desencadeadas são específicas de cada condição patológica analisada. As modificações nos elementos estudados sugerem alterações no padrão de migração intratímica e na exportação de timócitos, com comprometimento da função tímica, levando a maturação desequilibrada dos timócitos, com conseqüências para a resposta imune periférica.
Abstract: Thymus is the primary lymphoid organ responsible for differentiation of Tlymphocytes. This process is dependent of thymic microenvironment integrity and coordinated migration of hematopoietic precursors by chemokines and extracellular matrix elements. However, the literature shows that deep alterations in thymus microenvironment with modifications in thymocyte development may occur such as result of some pathological disorders. In this study we analyzed the atrophy induction and alterations in thymic microenvironment in three different models of thymus atrophy. We studied two models of infectious diseases, P.brasiliensis and P.berghei, and a metabolic disorder, alloxan induced diabetes. We have observed thymus atrophy in all models with different alterations levels in thymus microenvironment elements. Important molecules associated with intrathymic migration were been altered with significant modifications in extracellular matrix elements, chemokines and their specific receptors. Besides, ex vivo migration was altered in thymus atrophy induced by pathogenic agents, but no alterations were observed in diabetic mice suggesting that different pathological conditions studied, leads to singular alterations in thymus compartment. The modifications in thymic molecules observed in our models, suggest impaired thymus functionality and alterations in thymocyte migration patterns These alterations can lead T cell maturation imbalance with consequences in Tlymphocyte immune response.
Doutorado
Imunologia
Doutor em Genetica e Biologia Molecular
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Osorio, Tarazona José Manuel. "Del desorden al orden : el Fedón y la República como fuentes de la lógica teleológica en el Timeo." Master's thesis, Pontificia Universidad Católica del Perú, 2015. http://tesis.pucp.edu.pe/repositorio/handle/123456789/6032.

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Los relatos cosmológicos se pueden entender como el intento por responder a la pregunta acerca del nacimiento, desarrollo y evolución del universo . En la tradición filosófica griega y en la mitología se encuentran numerosos ejemplos de relatos cosmológicos que buscan hacer inteligible el proceso de desarrollo del universo. Los relatos teleológicos, por su parte, tratan de responder una pregunta distinta que los cosmológicos. En las explicaciones teleológicas se busca dar cuenta del destino del cosmos o el propósito específico por el cual el universo ha sido creado, sea este orden, bondad o belleza . Los diálogos teleológicos platónicos, el Timeo y la República, pueden ser entendido como el intento de reunir en una misma obra y discurso la explicación cosmológica y teleológica: dar razón del desarrollo del mundo a partir de la explicación del tránsito del desorden al orden que este exhibe en su estado final y el cual ha sido introducido por un agente externo al universo mismo, el demiurgo.
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Thalmann, Armin [Verfasser], Timo [Akademischer Betreuer] Leuders, and Timo [Gutachter] Leuders. "Mathematisches Wissen von Primarlehrpersonen / Armin Thalmann ; Gutachter: Timo Leuders ; Betreuer: Timo Leuders." Freiburg : Pädagogische Hochschule Freiburg, 2018. http://d-nb.info/1163448885/34.

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De, Santis Benedetta. "La transizione del documento da cartaceo a digitale: norma, tecnologie e strumenti a servizio della dematerializzazione secondo il Codice dell’Amministrazione Digitale." Master's thesis, Alma Mater Studiorum - Università di Bologna, 2013. http://amslaurea.unibo.it/5043/.

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Si vuole analizzare l’evoluzione della normativa e criticità che il Legislatore si è trovato ad affrontare durante la transizione da un contesto documentale cartaceo ad uno informatico, passando per sistemi ibridi, nell’ottica di incentivare l’informatizzazione e dematerializzazione delle procedure. Viene preso in considerazione l’intero ciclo di vita del documento, partendo dalla formazione (digitale o cartacea) fino alla sua conservazione, con particolare attenzione alle problematiche riscontrate dalle Pubbliche Amministrazioni in quanto produttori massivi di materiale documentale. Si toccheranno tematiche specifiche come la declinazione in ambito digitale della firma, ovvero le firme elettroniche, remote, massive, timbro digitale. Verranno approfonditi gli aspetti legali e problematiche correlate alla protocollazione ed archiviazione.
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Books on the topic "Timavo"

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Timano-Uralʹskiĭ treugolʹnik. Syktyvkar: Komi respublikanskai︠a︡ tipografii︠a︡, 2005.

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Pozdeev, I. A., and N. N. Gerasimov. Bolʹshai͡a neftʹ Timano-Pechory. Syktyvkar: Komi respublikanskai͡a tip., 2009.

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Timawa. Quezon City: Bughaw, 2019.

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Plato. Timaios. Athe na: Zacharopulos, 2004.

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Plato. Timaios. Athēna: Polis, 1995.

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Plato. Timaios. Hamburg: F. Meiner, 1992.

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Moskalenko, Mykhaĭlo. Srednedevonskie ostrakody Timano-Pechorskoĭ provint︠s︡ii. Sankt-Peterburg: Izd-vo Sankt-Peterburgskoĭ kartograficheskoĭ fabriki VSEGEI, 2001.

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K, Bazhenova T., ed. Organicheskai︠a︡ geokhimii︠a︡ Timano-Pechorskogo basseĭna. Sankt-Peterburg: VNIGRI, 2008.

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I︠U︡shkin, N. P. Biostratigrafii︠a︡ fanerozoi︠a︡ Timano-Pecherskoĭ provint︠s︡ii. Syktyvkar: Akademii︠a︡ nauk SSSR, Uralʹskoe otd-nie, Komi nauch. t︠s︡entr, 1989.

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K, Bazhenova T., ed. Organicheskai︠a︡ geokhimii︠a︡ Timano-Pechorskogo basseĭna. Sankt-Peterburg: VNIGRI, 2008.

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Book chapters on the topic "Timavo"

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Zajac, Peter. "Timrava." In Kindlers Literatur Lexikon (KLL), 1. Stuttgart: J.B. Metzler, 2020. http://dx.doi.org/10.1007/978-3-476-05728-0_21110-1.

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Sako-Hoess, Renata. "Timrava: Ťapákovci." In Kindlers Literatur Lexikon (KLL), 1–2. Stuttgart: J.B. Metzler, 2020. http://dx.doi.org/10.1007/978-3-476-05728-0_21111-1.

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Mannsperger, Dietrich, and Heinz-Günther Nesselrath. "Platon: Timaios." In Kindlers Literatur Lexikon (KLL), 1–2. Stuttgart: J.B. Metzler, 2020. http://dx.doi.org/10.1007/978-3-476-05728-0_15201-1.

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Kogarko, L. N., V. A. Konova, M. P. Orlova, and A. R. Woolley. "Kanin-Timan." In Alkaline Rocks and Carbonatites of the World, 46–48. Dordrecht: Springer Netherlands, 1995. http://dx.doi.org/10.1007/978-94-011-0513-2_5.

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Münzová, Alma. "Slančíková, Božena (Ps. Timrava)." In Metzler Autorinnen Lexikon, 500–501. Stuttgart: J.B. Metzler, 1998. http://dx.doi.org/10.1007/978-3-476-03702-2_348.

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Dimmendaal, Gerrit J. "Tima." In Studies in Language Companion Series, 331–53. Amsterdam: John Benjamins Publishing Company, 2009. http://dx.doi.org/10.1075/slcs.110.14dim.

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Nikolaou, Sousanna-Maria. "Platons „Timaios“ und Demokrits Atomlehre." In Die Atomlehre Demokrits und Platons Timaios, 140–93. Wiesbaden: Vieweg+Teubner Verlag, 1998. http://dx.doi.org/10.1007/978-3-663-12032-2_7.

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Krüger, Timmo. "Mehr Fortschritt wagen? Eine essayistische Kritik der Wette auf grünes Wachstum." In Soziale Bewegung und Protest, 63–80. Bielefeld, Germany: transcript Verlag, 2022. http://dx.doi.org/10.14361/9783839463000-004.

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Timmo Krüger interpretiert in seinem Beitrag die regierungspolitische Hoffnung auf grünes Wachstum als klimapolitische Variante einer Faustischen Wette. Er arbeitet heraus, weshalb der Faustische Weg des Kolonialismus und der Naturbeherrschung in der Dichtung gescheitert ist und auch in der Realität misslingen wird. Alternativ schlägt Timmo Krüger vor, den Zwang zum Fortschritt hinter uns zu lassen, unserer Abhängigkeit von Natur gewahr zu werden und uns auf Regelungen der kollektiven Selbstbeschränkung zu einigen, die Gleichheit und Freiheit für alle bieten. Er plädiert für die Wiederaneignung einer solidarischen Kultur der Selbstbeschränkung, in der Praktiken des Teilens und der demokratischen Selbstorganisation gelebt werden.
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Seemüller, Johannes. "Timo Hildebrand." In Am Limit – Wie Sportstars Krisen meistern, 143–64. Berlin, Heidelberg: Springer Berlin Heidelberg, 2021. http://dx.doi.org/10.1007/978-3-662-62552-1_8.

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Neumann, Stephanie. "Timrava ↗ Slančiková, Božena / Tlali, Miriam." In Metzler Autorinnen Lexikon, 537–39. Stuttgart: J.B. Metzler, 1998. http://dx.doi.org/10.1007/978-3-476-03702-2_373.

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Conference papers on the topic "Timavo"

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Bashirov, Ayrat, Ilya Galas, Marat Nazyrov, Dmitry Kuznetsov, and Azamat Akkuzhin. "Directional Radial Drilling Increases Reservoir Coverage with Precise Wellbore Placement Resulting in a Significant Production Increase from a Thin Reservoir." In Abu Dhabi International Petroleum Exhibition & Conference. SPE, 2021. http://dx.doi.org/10.2118/208035-ms.

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Abstract In many oil and gas provinces not only in Russia, but throughout the world, carbonate strata make up a significant portion of the sedimentary cover, and large accumulations of hydrocarbons are associated with them. However, the purposeful study of them as reservoirs for hydrocarbons in our country practically began only in the post-war years. In the special petrography laboratory carbonate rocks composing various stratigraphic complexes of almost all oil and gas provinces of the Soviet Union were studied, and in particular, Paleozoic carbonate strata of the Timan-Pechora province, Ural-Volga region, Belarus, Kazakhstan, ancient Riphean-Cambrian formations of Yakutia and relatively young strata of the Late Cretaceous of the northeastern Ciscaucasia. Carbonates are widespread sedimentary rocks. A very significant part of them was formed in the conditions of vast shallow-water marine epicontinental basins. A large number of works are devoted to the study of such deposits. However, issues related to the conditions of formation of carbonate sediments and their postsedimentary changes cannot be considered resolved, as well as the classification of the rocks themselves. The analyzed field is the Osvanyurskoye one. It was discovered in 2007. The field is located in the north-east of the European part of the Russian Federation, 2 km from Usinsk in the Komi Republic. The field is a part of the Timano-Pechora oil and gas province and it is a mature field (fig. 1). The objective was a 2.5m thick layer of the Serpukhov horizon.
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Elbadawi, Khalid, and Ehab Al-Shaer. "TimeVM." In the 4th International Symposium. New York, New York, USA: ACM Press, 2009. http://dx.doi.org/10.1145/1533057.1533077.

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"Termoliz asfaltenov bitumov voyskogo mestorozhdeniya timano-pechorskoy provintsii." In Perspektivnye materialy s ierarkhicheskoy strukturoy dlya novykh tekhnologiy i nadezhnykh konstruktsiy, Khimiya nefti i gaza. Tomsk State University, 2018. http://dx.doi.org/10.17223/9785946217408/421.

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"Produkty piroliza kerogena domanikovykh otlozheniy timano-pechorskogo osadochnogo basseyna." In Perspektivnye materialy s ierarkhicheskoy strukturoy dlya novykh tekhnologiy i nadezhnykh konstruktsiy, Khimiya nefti i gaza. Tomsk State University, 2018. http://dx.doi.org/10.17223/9785946217408/447.

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Akhkubekov, Alexander Eduardovich, and Vladimir Vasiliev. "Acid Tunneling Technology: Application Potential in Timano-Pechora Carbonates." In SPE Russian Oil and Gas Conference and Exhibition. Society of Petroleum Engineers, 2010. http://dx.doi.org/10.2118/135989-ms.

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"Geokhimiya neftey i organicheskogo veshchestva paleozoya timano- pechorskogo neftegazonosnogo basseyna." In Perspektivnye materialy s ierarkhicheskoy strukturoy dlya novykh tekhnologiy i nadezhnykh konstruktsiy, Khimiya nefti i gaza. Tomsk State University, 2018. http://dx.doi.org/10.17223/9785946217408/440.

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Prischepa, O., E. Grokhotov, I. Makarova, O. Averyanova, and V. Nikiforova. "Petroleum Prospects of the Domanik Formation in Timano-Pechora Province." In Saint Petersburg 2018. Netherlands: EAGE Publications BV, 2018. http://dx.doi.org/10.3997/2214-4609.201800174.

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Bushnev, D., N. Burdelnaya, and A. Derevesnikova. "HYDROCARBONS-BIOMARKERS OF PARAFFIN OILS OF THE TIMANO-PECHORA BASIN." In New Challenges in Fundamental and Applied Petroleum Geology. Novosibirsk State University, 2021. http://dx.doi.org/10.25205/978-5-4437-1248-2-101-103.

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Xu, Wanru, Panlong Yang, Chaocan Xiang, and Chang Tian. "TIMAO: Time-Sensitive Mobile Advertisement Offloading with Performance Guarantee." In 2018 IEEE 24th International Conference on Parallel and Distributed Systems (ICPADS). IEEE, 2018. http://dx.doi.org/10.1109/padsw.2018.8644857.

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Faizov, Yuri, Olesya Vladimirovna Levanyuk, Diankui Fu, Olga Ivanova, Bernhard R. Lungwitz, and Kevin D. Mauth. "Challenges and Solutions of Stimulating Carbonate Reservoirs in Timano-Pechora, Russia." In OTC Brasil. Offshore Technology Conference, 2011. http://dx.doi.org/10.4043/22257-ms.

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Reports on the topic "Timavo"

1

SGC, Servicio Geológico Colombiano. Geología de la plancha 364 Timbio. Escala 1:100.000. Producto. Versión año 1996. Bogotá: Servicio Geológico Colombiano, January 1996. http://dx.doi.org/10.32685/10.143.1996.796.

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SGC, Servicio Geológico Colombiano. Mapa Geomorfológico aplicado a movimientos en masa escala 1:100.000. Plancha 364 Timbío. Producto. Bogotá: Servicio Geológico Colombiano, May 2014. http://dx.doi.org/10.32685/4.7.2014.457.

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SGC, Servicio Geológico Colombiano. Mapa Geomorfológico aplicado a movimientos en masa escala 1:100.000. Plancha 389 Timaná (Suaza). Producto. Bogotá: Servicio Geológico Colombiano, November 2015. http://dx.doi.org/10.32685/4.7.2015.742.

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SGC, Servicio Geológico Colombiano. Zonificación de la susceptibilidad y la amenaza relativa por movimientos en masa escala 1:100.000. Plancha 364 Timbío. Producto. Bogotá: Servicio Geológico Colombiano, May 2014. http://dx.doi.org/10.32685/4.7.2014.40.

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SGC, Servicio Geológico Colombiano. Geología de la Planchas 367 Gigante, 368 San Vicente del Caguán, 389 Timaná, 390 Puerto Rico, 391 Lusitania y 414 El Doncello - Departamentos de Caquetá y Huila. Escala 1:100.000. Producto. Versión año 2003. Bogotá: Servicio Geológico Colombiano, January 2003. http://dx.doi.org/10.32685/10.143.2003.442.

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de Caritat, Patrice, Brent McInnes, and Stephen Rowins. Towards a heavy mineral map of the Australian continent: a feasibility study. Geoscience Australia, 2020. http://dx.doi.org/10.11636/record.2020.031.

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Heavy minerals (HMs) are minerals with a specific gravity greater than 2.9 g/cm3. They are commonly highly resistant to physical and chemical weathering, and therefore persist in sediments as lasting indicators of the (former) presence of the rocks they formed in. The presence/absence of certain HMs, their associations with other HMs, their concentration levels, and the geochemical patterns they form in maps or 3D models can be indicative of geological processes that contributed to their formation. Furthermore trace element and isotopic analyses of HMs have been used to vector to mineralisation or constrain timing of geological processes. The positive role of HMs in mineral exploration is well established in other countries, but comparatively little understood in Australia. Here we present the results of a pilot project that was designed to establish, test and assess a workflow to produce a HM map (or atlas of maps) and dataset for Australia. This would represent a critical step in the ability to detect anomalous HM patterns as it would establish the background HM characteristics (i.e., unrelated to mineralisation). Further the extremely rich dataset produced would be a valuable input into any future machine learning/big data-based prospectivity analysis. The pilot project consisted in selecting ten sites from the National Geochemical Survey of Australia (NGSA) and separating and analysing the HM contents from the 75-430 µm grain-size fraction of the top (0-10 cm depth) sediment samples. A workflow was established and tested based on the density separation of the HM-rich phase by combining a shake table and the use of dense liquids. The automated mineralogy quantification was performed on a TESCAN® Integrated Mineral Analyser (TIMA) that identified and mapped thousands of grains in a matter of minutes for each sample. The results indicated that: (1) the NGSA samples are appropriate for HM analysis; (2) over 40 HMs were effectively identified and quantified using TIMA automated quantitative mineralogy; (3) the resultant HMs’ mineralogy is consistent with the samples’ bulk geochemistry and regional geological setting; and (4) the HM makeup of the NGSA samples varied across the country, as shown by the mineral mounts and preliminary maps. Based on these observations, HM mapping of the continent using NGSA samples will likely result in coherent and interpretable geological patterns relating to bedrock lithology, metamorphic grade, degree of alteration and mineralisation. It could assist in geological investigations especially where outcrop is minimal, challenging to correctly attribute due to extensive weathering, or simply difficult to access. It is believed that a continental-scale HM atlas for Australia could assist in derisking mineral exploration and lead to investment, e.g., via tenement uptake, exploration, discovery and ultimately exploitation. As some HMs are hosts for technology critical elements such as rare earth elements, their systematic and internally consistent quantification and mapping could lead to resource discovery essential for a more sustainable, lower-carbon economy.
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