Fer mapes per conèixer la Història: aportacions de la cartografia a l'estudi de l'Alta Edat Mitjana

To make maps to know history: contributions from the cartography to the study of the early middle ages. The accomplishment of maps can allow us to know many aspects that documents written do not allow us to have knowledge. This paper focuses on the boundaries of the townships or the parishes, on the routes and ways, and on the place names or on the invocations of the churches, in order to get to know like it was the territory in the early medieval centuries. One reaches the conclusion that often the limits, the ways and the settlements were created at early middle ages. This study allows to raise the ruptures and the continuities that took place throughout these centuries in the settlement.

Monitorizacion de los cambios de uso del suelo en la cabecera de cuenca de la ribera salada mediante fotografía aérea y S.I.G. (El Solsonès, Lleida, España)

Durante estos últimos 50 años ha tenido lugar un abandono de las masías y de los cultivos tradicionales en los Prepirineos catalanes. En este trabajo se han estudiado los cambios de usos del suelo desde los años 50 hasta la actualidad en una cuenca de 6577 ha situada en la cabecera de la Ribera Salada (El Solsonès). Para ello se han utilizado fotografías aéreas del año 1957 y del año 1992. Como base cartográfica sirvieron los ortofotomapas del año 1993. El análisis de los cambios de usos según diferentes variables (pendiente y orientación) y según diferentes enfoques (intensidad del cambio y uso final), se ha llevado a cabo mediante el programa de SIG ARC/INFO®. Se han establecido tendencias en la evolución de los usos según la pendiente y la orientación. Los resultados obtenidos muestran que los campos de cultivo son los que han disminuido más en superficie, dando lugar a pastos. Por otro lado, el bosque denso ha aumentado considerablemente su extensión (845 ha).

Els assentaments de les edats del bronze, ibèrica i romana d"Els Llirians del Mas i Les Torres (Salàs de Pallars, Pallars Jussà)

[cat] En els anys 2003 i 2004 una intervenció arqueològica preventiva en el terme de Salàs de Pallars va permetre documentar seixanta estructures excavades al subsòl. La majoria de les estructures foren identificades com a sitges, però també es documentaren cubetes i fosses de diversa funció, algunes utilitzades com a sepultures. L"estudi dels materials recuperats, complementats per datacions radiocarbòniques, indiquen dos períodes cronològics: el bronze inicial i l"etapa ibèrica plena, als quals s"ha d"afegir una única estructura que pertany a començaments de l"Imperi romà. Les dades obtingudes informen sobre les pràctiques de les comunitats agrícoles assentades en el sector meridional de la comarca del Pallars Jussà en tres moments històrics diferents. [eng]In 2003 and 2004 a Preventive Archaeological Excavation was done in the locality of Salàs de Pallars. This allowed to catalogue the sixty structures found in the subsoil. Most of the structures were identified as silos, but we also documented basins and pits with different functions, some used as graves. The study of the recovered materials, supported by a radiocarbon analysis technique, ages this around two chronological periods: the Early Bronze Age and Iberian Period. We must add a third period to classify a single structure that belongs to the Early Roman Empire. The obtained results provide us information about the farming methods used by the communities placed in the southern Region of the Pallars Jussà during the three different historical moments.

Meeting report of the European mouse complex genetics network SYSGENET.

The second scientific meeting of the European systems genetics network for the study of complex genetic human disease using genetic reference populations (SYSGENET) took place at the Center for Cooperative Research in Biosciences in Bilbao, Spain, December 10-12, 2012. SYSGENET is funded by the European Cooperation in the Field of Scientific and Technological Research (COST) and represents a network of scientists in Europe that use mouse genetic reference populations (GRPs) to identify complex genetic factors influencing disease phenotypes (Schughart, Mamm Genome 21:331-336, 2010). About 50 researchers working in the field of systems genetics attended the meeting, which consisted of 27 oral presentations, a poster session, and a management committee meeting. Participants exchanged results, set up future collaborations, and shared phenotyping and data analysis methodologies. This meeting was particularly instrumental for conveying the current status of the US, Israeli, and Australian Collaborative Cross (CC) mouse GRP. The CC is an open source project initiated nearly a decade ago by members of the Complex Trait Consortium to aid the mapping of multigenetic traits (Threadgill, Mamm Genome 13:175-178, 2002). In addition, representatives of the International Mouse Phenotyping Consortium were invited to exchange ongoing activities between the knockout and complex genetics communities and to discuss and explore potential fields for future interactions.

Rockfall susceptibility assessment and remote geological mapping with LiDAR point clouds

Characterizing the geological features and structures in three dimensions over inaccessible rock cliffs is needed to assess natural hazards such as rockfalls and rockslides and also to perform investigations aimed at mapping geological contacts and building stratigraphy and fold models. Indeed, the detailed 3D data, such as LiDAR point clouds, allow to study accurately the hazard processes and the structure of geologic features, in particular in vertical and overhanging rock slopes. Thus, 3D geological models have a great potential of being applied to a wide range of geological investigations both in research and applied geology projects, such as mines, tunnels and reservoirs. Recent development of ground-based remote sensing techniques (LiDAR, photogrammetry and multispectral / hyperspectral images) are revolutionizing the acquisition of morphological and geological information. As a consequence, there is a great potential for improving the modeling of geological bodies as well as failure mechanisms and stability conditions by integrating detailed remote data. During the past ten years several large rockfall events occurred along important transportation corridors where millions of people travel every year (Switzerland: Gotthard motorway and railway; Canada: Sea to sky highway between Vancouver and Whistler). These events show that there is still a lack of knowledge concerning the detection of potential rockfalls, making mountain residential settlements and roads highly risky. It is necessary to understand the main factors that destabilize rocky outcrops even if inventories are lacking and if no clear morphological evidences of rockfall activity are observed. In order to increase the possibilities of forecasting potential future landslides, it is crucial to understand the evolution of rock slope stability. Defining the areas theoretically most prone to rockfalls can be particularly useful to simulate trajectory profiles and to generate hazard maps, which are the basis for land use planning in mountainous regions. The most important questions to address in order to assess rockfall hazard are: Where are the most probable sources for future rockfalls located? What are the frequencies of occurrence of these rockfalls? I characterized the fracturing patterns in the field and with LiDAR point clouds. Afterwards, I developed a model to compute the failure mechanisms on terrestrial point clouds in order to assess the susceptibility to rockfalls at the cliff scale. Similar procedures were already available to evaluate the susceptibility to rockfalls based on aerial digital elevation models. This new model gives the possibility to detect the most susceptible rockfall sources with unprecented detail in the vertical and overhanging areas. The results of the computation of the most probable rockfall source areas in granitic cliffs of Yosemite Valley and Mont-Blanc massif were then compared to the inventoried rockfall events to validate the calculation methods. Yosemite Valley was chosen as a test area because it has a particularly strong rockfall activity (about one rockfall every week) which leads to a high rockfall hazard. The west face of the Dru was also chosen for the relevant rockfall activity and especially because it was affected by some of the largest rockfalls that occurred in the Alps during the last 10 years. Moreover, both areas were suitable because of their huge vertical and overhanging cliffs that are difficult to study with classical methods. Limit equilibrium models have been applied to several case studies to evaluate the effects of different parameters on the stability of rockslope areas. The impact of the degradation of rockbridges on the stability of large compartments in the west face of the Dru was assessed using finite element modeling. In particular I conducted a back-analysis of the large rockfall event of 2005 (265'000 m3) by integrating field observations of joint conditions, characteristics of fracturing pattern and results of geomechanical tests on the intact rock. These analyses improved our understanding of the factors that influence the stability of rock compartments and were used to define the most probable future rockfall volumes at the Dru. Terrestrial laser scanning point clouds were also successfully employed to perform geological mapping in 3D, using the intensity of the backscattered signal. Another technique to obtain vertical geological maps is combining triangulated TLS mesh with 2D geological maps. At El Capitan (Yosemite Valley) we built a georeferenced vertical map of the main plutonio rocks that was used to investigate the reasons for preferential rockwall retreat rate. Additional efforts to characterize the erosion rate were made at Monte Generoso (Ticino, southern Switzerland) where I attempted to improve the estimation of long term erosion by taking into account also the volumes of the unstable rock compartments. Eventually, the following points summarize the main out puts of my research: The new model to compute the failure mechanisms and the rockfall susceptibility with 3D point clouds allows to define accurately the most probable rockfall source areas at the cliff scale. The analysis of the rockbridges at the Dru shows the potential of integrating detailed measurements of the fractures in geomechanical models of rockmass stability. The correction of the LiDAR intensity signal gives the possibility to classify a point cloud according to the rock type and then use this information to model complex geologic structures. The integration of these results, on rockmass fracturing and composition, with existing methods can improve rockfall hazard assessments and enhance the interpretation of the evolution of steep rockslopes. -- La caractérisation de la géologie en 3D pour des parois rocheuses inaccessibles est une étape nécessaire pour évaluer les dangers naturels tels que chutes de blocs et glissements rocheux, mais aussi pour réaliser des modèles stratigraphiques ou de structures plissées. Les modèles géologiques 3D ont un grand potentiel pour être appliqués dans une vaste gamme de travaux géologiques dans le domaine de la recherche, mais aussi dans des projets appliqués comme les mines, les tunnels ou les réservoirs. Les développements récents des outils de télédétection terrestre (LiDAR, photogrammétrie et imagerie multispectrale / hyperspectrale) sont en train de révolutionner l'acquisition d'informations géomorphologiques et géologiques. Par conséquence, il y a un grand potentiel d'amélioration pour la modélisation d'objets géologiques, ainsi que des mécanismes de rupture et des conditions de stabilité, en intégrant des données détaillées acquises à distance. Pour augmenter les possibilités de prévoir les éboulements futurs, il est fondamental de comprendre l'évolution actuelle de la stabilité des parois rocheuses. Définir les zones qui sont théoriquement plus propices aux chutes de blocs peut être très utile pour simuler les trajectoires de propagation des blocs et pour réaliser des cartes de danger, qui constituent la base de l'aménagement du territoire dans les régions de montagne. Les questions plus importantes à résoudre pour estimer le danger de chutes de blocs sont : Où se situent les sources plus probables pour les chutes de blocs et éboulement futurs ? Avec quelle fréquence vont se produire ces événements ? Donc, j'ai caractérisé les réseaux de fractures sur le terrain et avec des nuages de points LiDAR. Ensuite, j'ai développé un modèle pour calculer les mécanismes de rupture directement sur les nuages de points pour pouvoir évaluer la susceptibilité au déclenchement de chutes de blocs à l'échelle de la paroi. Les zones sources de chutes de blocs les plus probables dans les parois granitiques de la vallée de Yosemite et du massif du Mont-Blanc ont été calculées et ensuite comparés aux inventaires des événements pour vérifier les méthodes. Des modèles d'équilibre limite ont été appliqués à plusieurs cas d'études pour évaluer les effets de différents paramètres sur la stabilité des parois. L'impact de la dégradation des ponts rocheux sur la stabilité de grands compartiments de roche dans la paroi ouest du Petit Dru a été évalué en utilisant la modélisation par éléments finis. En particulier j'ai analysé le grand éboulement de 2005 (265'000 m3), qui a emporté l'entier du pilier sud-ouest. Dans le modèle j'ai intégré des observations des conditions des joints, les caractéristiques du réseau de fractures et les résultats de tests géoméchaniques sur la roche intacte. Ces analyses ont amélioré l'estimation des paramètres qui influencent la stabilité des compartiments rocheux et ont servi pour définir des volumes probables pour des éboulements futurs. Les nuages de points obtenus avec le scanner laser terrestre ont été utilisés avec succès aussi pour produire des cartes géologiques en 3D, en utilisant l'intensité du signal réfléchi. Une autre technique pour obtenir des cartes géologiques des zones verticales consiste à combiner un maillage LiDAR avec une carte géologique en 2D. A El Capitan (Yosemite Valley) nous avons pu géoréferencer une carte verticale des principales roches plutoniques que j'ai utilisé ensuite pour étudier les raisons d'une érosion préférentielle de certaines zones de la paroi. D'autres efforts pour quantifier le taux d'érosion ont été effectués au Monte Generoso (Ticino, Suisse) où j'ai essayé d'améliorer l'estimation de l'érosion au long terme en prenant en compte les volumes des compartiments rocheux instables. L'intégration de ces résultats, sur la fracturation et la composition de l'amas rocheux, avec les méthodes existantes permet d'améliorer la prise en compte de l'aléa chute de pierres et éboulements et augmente les possibilités d'interprétation de l'évolution des parois rocheuses.

La crisis del segle III a l’àrea compresa entre Tarraco i Saguntum: aproximació a partir de les dades arqueològiques

The purpose of this work is to evaluate the possible impact of the so-called “crisis of the 3rd century” in the area between Tarraco (Tarragona) and Saguntum (Sagunt), currently corresponding to the southern limit of Catalonia and the north of Valencia, which during the Roman era made up the southernmost part of the conventus Tarraconensis. The processes of change experienced in rural settlements and cities between the Severan dynasty and the beginning of the tetrarchy are analyzed, and the importance of the city-country relationship is examined to explain these changes. The extent of the Frankish invasion during of the Gallic period, initially substantiated by sources and now by archaeological evidence, is discussed. The study of coin hoards (treasures and deposits) from the second half of the 3rd century, found in abundance in this area, is a very interesting aspect of this topic. In addition, a quantitative approach is used to study the population changes experienced as a result of the rural settlement of this area during the 3rd century, between the High and the Low Empires.

El poblament tardoantic al sector meridional de la Tarraconensis (sud de Catalunya i nord del País Valencià). Concomitàncies i diferències

Les darreres recerques dutes a terme en el Projecte Ager Tarraconensis (PAT) han permès augmentar considerablement els coneixements existents sobre l’antiguitat tardana al territorium de Tarraco, tema que ja havíem estudiat parcialment en la nostra tesi doctoral (1992), que inclou també altres àrees del Camp de Tarragona no incloses al PAT. D’altra banda, en els darrers anys hem tingut també ocasió d’estudiar parcialment el poblament antic a la zona de les terres de l’Ebre i al nord del País Valencià, molt especialment a les comarques de l’Alt Palància i la Plana de Castelló. El conjunt d’aquests estudis ens permet plantejar una visió general sobre el poblament tardoantic en una zona determinada que correspon a la part costanera meridional de l’antiga provincia Tarraconensis, amb els límits i la denominació que rep a partir de la divisió de Dioclecià. L’estudi comparatiu del poblament tardoantic d’aquestes àrees permet contrastar, a més de punts en comú, també algunes diferències, tant en el diferent grau de pervivència dels hàbitats després de la crisi del segle III com en l’aparició de nous tipus d’hàbitats (poblats en altura) que no apareixen en totes les àrees, sinó només en les més meridionals. S’aborda també la problemàtica de l’existència d’unes poques vil·les luxoses durant el segle IV (especialment la controvertida de Centcelles), en contrast amb altres hàbitats més modestos, així com el pas de la vil·la a un altre tipus de poblament dispers.

Feasibility Study and Market Review of Small Scale Bioenergy Heating Plants in North-West Russia

The paper is focused on feasibility study and market review of small scale bioenergy heating plants in the Russian North-West region. The main focus is effective and competitive usage of low-grade wood for heating purposes in the region. As example of economical feasibility estimation it was chosen the project of reconstruction of small scale boiler plant in Leningrad region that Brofta Oy is planning to implement the nearest time. It includes calculation the payback time with and without interest, the estimation of probable investments, the evaluation of possible risks and research on the potential of small scale heating plants projects. Calculations show that the profitability of this kind of projects is high, but payback time is not very short, because of high level of initial investments. Though, the development of small scale bioenergy heating plants in the region is considered to be the best way to solve the problems of heat supply in small settlements using own biomass resources.

Rakennukset ja rakentajat Raision Ihalassa rautakauden lopulla ja varhaisella keskiajalla

Turun yliopiston arkeologian oppiaine tutki Raision Ihalan historiallisella kylätontilla, ns. Mullin eduspellolla, asuinpaikan, josta löydettiin maamme oloissa harvinaisen hyvin säilyneitä rakennusten puuosien jäännöksiä. Löytö on ainutlaatuinen Suomen oloissa ja sillä on kansainvälistäkin merkitystä, koska hyvin säilyneet myöhemmän rautakauden ja varhaisen keskiajan maaseutuasuinpaikat, joista tavataan puujäännöksiä, ovat harvinaisia erityisesti itäisen Itämeren piirissä. Rakennukset on ennallistettu käyttäen tiukkaa paikallisen analogian (’Tight Local Analogy’) metodia, erityisesti suoraa historiallista analogista lähestymistapaa. Tätä tarkoitusta varten muodostettiin aluksi arkeologinen, historiallinen ja etnografinen lähdemalli. Tämä valittiin maantieteellisesti ja ajallisesti relevantista tutkimusaineistosta pohjoisen Itämeren piiristä. Tiedot lounaisen Suomen rakennuksista ja rakennusteknologiasta katsottiin olevan tärkein osa mallia johtuen historiallisesta ja spatiaalisesta jatkuvuudesta. Lähdemalli yhdistettiin sitten Mullin arkeologiseen aineistoon ja analyysin tuloksena saatiin rakennusten ennallistukset. Mullista on voitu ennallistaa ainakin kuusi eri rakennusta neljässä eri rakennuspaikassa. Rakennusteknologia perustui kattoa kannattaviin horisontaalisiin pitkiin seinähirsiin, jotka oli nurkissa yhdistetty joko salvoksella tai varhopatsaalla. Kaikissa rakennuksissa ulkoseinän pituus oli 5 – 7 metriä. Löydettiin lisäksi savi- ja puulattioita sekä kaksi tulisijaa, savikupoliuuni ja avoin liesi. Runsaan palaneen saven perusteella on mahdollista päätellä, että katto oli mitä todennäköisimmin kaksilappeinen vuoliaiskatto, joka oli katettu puulla ja/tai turpeella. Kaikki rakennukset olivat samaa tyyppiä ja ne käsittivät isomman huoneen ja kapean eteisen. Kaikki analysoitu puu oli mäntyä. Ulkoalueelta tavattiin lisäksi tunkioita, ojia, aitoja ja erilaisia varastokuoppia. Rakennukset on ajoitettu 900-luvun lopulta 1200-luvun lopulle (cal AD). Lopuksi tutkittiin rakennuksia yhteisöllisessä ympäristössään, niiden ajallista asemaa sekä asukkaiden erilaisia spatiaalisia kokemuksia ja yhteyksiä. Raision Ihalaa analysoidaan sosiaalisen identiteetin ja sen materiaalisten ilmenemismuotojen kautta. Nämä sosiaaliset identiteetit muodostuvat kommunikaatioverkostoista eri spatiaalisilla ja yhteisöllisillä ta¬soilla. Näitä eri tasoja ovat: 1) kotitalous arjen toimintoineen, perhe ja sukulaisuussuhteet traditioineen; 2) paikallinen identiteetti, rakennus, rakennuspaikka, asuinpaikan ympäristö ja sen käyttö, (maa)talo ja kylä; 3) Raision Ihalan kylä laajemmassa alueellisessa kontekstissaan pohjoisen Itämeren piirissä: kauppiaiden ja käsityöläisten kontaktiverkostot, uskonnollinen identiteetti ja sen muutokset.

El territorio y la ciudad de Tarraco

This paper presents a brief description of the archaeological research in the territory and in the city of Tarraco, the ancient capital of provincia Hispania Tarraconensis and one of the main centres for the spread of Hispanic Christianity. Althoug Tarraco was the last capital under imperial control and the firs Hispanic metropolitan see, the city had only a secondary role by comparison with other Hispanic cities during late antiquity. This evolution shaped the development of Tarraco during the 7th century, but archaeologists identify an important architectural vitality still in the 6th century at the same time as other episcopal cities were evolving. During this period, the final Christianization of the symbolic spaces of ancient paganism took place, establishing the ideological basis of medieval urbanism that is still preserved today. The paper also interprets the sites through raising key questions as well as describing rural settlements, where archaeological knowledge is not so far advanced, due in part to the difficult nature of archaeological research, and in part to the need to study new construcitve models, as well as to the systematic collection of the relevant material culture.

Financial integration and TARGET2-Securities – A stakeholder approach

The purpose of this study was to analyze how different stakeholders, such as the European Central Bank, the European Commission, the European Central Securities Depositories Association, the Bank of International Settlements and the International Monetary Fund, have influenced the European financial integration in the area of securities clearing and settlement since the introduction of the single currency. The results show that the contribution differs from stakeholder to another and can take the form of standards and recommendations, legislation, research and publications, risk analysis etc. The Eurosystem has been particularly active in this area by proving and planning central bank services, such as TARGET2, CCMB2 and T2S. Along the way the development has and continues to face challenges that need to be solved by European authorities. Coordination is a key factor for the future as we have seen during the recent financial turmoil.

Kirkkaasta sameaan : Meren kuormitus ja tila Saaristomerellä ja Ahvenanmaalla

Tässä raportissa tarkastellaan Saaristomeren ja Ahvenmaan merialueen kuormitusta ja tilaa ja niissä viime vuosikymmeninä tapahtuneita muutoksia vuosiin 2008 ja 2009 saakka. Pääpaino on ravinnekuormituksessa ja veden laadussa, mutta mukana on taustatietoa ja muun muassa katsaus kalakannoista. Saaristomeren ja Ahvenanmaan merialueen tila on heikentynyt huomattavasti viimeisten vuosikymmenten aikana. Erityisesti fosforin ja a-klorofyllin määrät ovat kasvaneet ja näkösyvyys pienenentynyt. Viimeisen kymmenen vuoden aikana pintaveden fosforipitoisuuden kasvu on laantunut suurimmassa osassa aluetta, mutta pohjanläheisessä vesikerroksessa ja talvella fosforipitoisuus on jatkanut kasvuaan monin paikoin viime vuosiin asti. Myös a-klorofyllin määrä on lisääntynyt ulko- ja välisaaristossa 2000-luvullakin. Viime vuosina klorofyllipitoisuuden kasvu on kuitenkin laantunut tai pitoisuus laskenut varsinkin rannikonläheisissä vesissä. Merialueen suurin paikallinen ravinnekuormittaja on maatalous, mutta varsinkin typpeä tulee runsaasti myös ilmalaskeumana. Sisäinen kuormitus ja virtausten mukana Suomenlahdelta ja muualta Itämereltä tulevat ravinteet heikentävät niin ikään merialueen tilaa. Muita ravinnelähteitä ovat mm. haja-asutus, jätevedenpuhdistamot ja kalankasvatus. Ahvenanmaan merialueelle ravinteita tulee enemmän muualta kuin Ahvenanmaalta. Hajakuormituksessa on tapahtunut viime vuosikymmeninä selviä vuodenaikaisia muutoksia. Vuosina 1990 – 2009 jokien mereen tuoma ravinne- ja kiintoainekuormitus on ollut talvisin ja syksyisin selvästi suurempaa kuin vuosina 1970 – 1989. Talviaikaisen kuormituksen lisääntyminen johtuu aiempaa lauhemmista talvista, ja antaa viitteitä ilmastonmuutoksen mukanaan tuomista muutoksista. Vaikka Saaristomeren ja Ahvenanmaan merialueen tilassa on ollut viime aikoina nähtävissä myönteisiäkin merkkejä, on niiden tila edelleen huolestuttava. Ainoa keino merialueen tilan parantamiseksi on kuormituksen huomattava vähentäminen. Vähentäminen koskee niin paikallisia ravinnelähteitä, erityisesti maataloutta, kuin muualta Itämereltä virtausten mukana tulevia ravinteita ja ilmalaskeumaa.

Nouvelle carte particulière de l'Amérique ou sont exactement marquées les provinces suivantes comme la Caroline Meridionale, la Floride, la Lousiane, le Mexique, le Jucatan, le Guatimala, le Darien & une partie de Cuba

Irtokartta

Investigation of the applicability of LVDC microgrids in utility distribution in Russia

The research towards efficient, reliable and environmental-friendly power supply solutions is producing growing interest to the “Smart Grid” approach for the development of the electricity networks and managing the increasing energy consumption. One of the novel approaches is an LVDC microgrid. The purpose of the research is to analyze the possibilities for the implementation of LVDC microgrids in public distribution networks in Russia. The research contains the analysis of the modern Russian electric power industry, electricity market, electricity distribution business, regulatory framework and standardization, related to the implementation of LVDC microgrid concept. For the purpose of the economic feasibility estimation, a theoretical case study for comparing low voltage AC and medium voltage AC with LVDC microgrid solutions for a small settlement in Russia is presented. The results of the market and regulatory framework analysis along with the economic comparison of AC and DC solutions show that implementation of the LVDC microgrid concept in Russia is possible and can be economically feasible. From the electric power industry and regulatory framework point of view, there are no serious obstacles for the LVDC microgrids in Russian distribution networks. However, the most suitable use cases at the moment are expected to be found in the electrification of remote settlements, which are isolated from the Unified Energy System of Russia.