29 research outputs found
Π Π°Π·ΡΠ°Π±ΠΎΡΠΊΠ° ΡΠΈΡΡΠ΅ΠΌΡ ΠΌΠ΅ΡΠΎΠΏΡΠΈΡΡΠΈΠΉ ΠΏΠΎ ΡΠΎΠ²Π΅ΡΡΠ΅Π½ΡΡΠ²ΠΎΠ²Π°Π½ΠΈΡ ΠΎΡΠ³Π°Π½ΠΈΠ·Π°ΡΠΈΠΎΠ½Π½ΠΎΠΉ ΠΊΡΠ»ΡΡΡΡΡ ΠΊΠΎΠΌΠΏΠ°Π½ΠΈΠΈ ΠΠΠ Β«ΠΠ°ΡΡΡ-Π’ΠΎΠΌΡΠΊΒ»
ΠΠΊΡΡΠ°Π»ΡΠ½ΠΎΡΡΡ ΠΏΡΠΎΠ±Π»Π΅ΠΌΡ ΡΠΎΡΠΌΠΈΡΠΎΠ²Π°Π½ΠΈΡ ΠΎΡΠ³Π°Π½ΠΈΠ·Π°ΡΠΈΠΎΠ½Π½ΠΎΠΉ ΠΊΡΠ»ΡΡΡΡΡ ΠΎΠ΄Π½Π° ΠΈΠ· Π²Π΅ΡΠΎΠΌΡΡ
Π² ΠΊΠΎΠΌΠΏΠ°Π½ΠΈΠΈ, ΡΠ°ΠΊ ΠΊΠ°ΠΊ ΠΎΡ ΡΠ΅ΡΠΊΠΎΠΉ ΡΡΡΡΠΊΡΡΡΡ ΠΎΡΠ³Π°Π½ΠΈΠ·Π°ΡΠΈΠΎΠ½Π½ΠΎΠΉ ΠΊΡΠ»ΡΡΡΡΡ Π·Π°Π²ΠΈΡΠΈΡ Π½Π΅ ΡΠΎΠ»ΡΠΊΠΎ Π±Π»Π°Π³ΠΎΠΏΡΠΈΡΡΠ½ΠΎΠ΅ ΡΡΡΠ΅ΡΡΠ²ΠΎΠ²Π°Π½ΠΈΠ΅ Π² ΠΎΡΠ³Π°Π½ΠΈΠ·Π°ΡΠΈΠΈ, ΠΏΠΎΠ²ΡΡΠ΅Π½ΠΈΠ΅ ΠΏΡΠΎΡΠ΅ΡΡΠΈΠΎΠ½Π°Π»ΠΈΠ·ΠΌΠ° ΠΈ ΡΠ²ΠΎΡΡΠ΅ΡΡΠ²Π° ΡΠΎΡΡΡΠ΄Π½ΠΈΠΊΠΎΠ², Π½ΠΎ ΠΈ ΠΊΠΎΠ½Π΅ΡΠ½ΡΠΉ ΡΠ΅Π·ΡΠ»ΡΡΠ°Ρ Π΄Π΅ΡΡΠ΅Π»ΡΠ½ΠΎΡΡΠΈ ΠΊΠΎΠΌΠΏΠ°Π½ΠΈΠΈ. ΠΠ±ΡΠ΅ΠΊΡΠΎΠΌ ΠΈΡΡΠ»Π΅Π΄ΠΎΠ²Π°Π½ΠΈΡ ΡΠ²Π»ΡΠ΅ΡΡΡ ΠΊΠΎΠΌΠΏΠ°Π½ΠΈΡ ΠΠΠ Β«ΠΠ°ΡΡΡ β Π’ΠΎΠΌΡΠΊΒ». ΠΡΠ΅Π΄ΠΌΠ΅ΡΠΎΠΌ ΠΈΡΡΠ»Π΅Π΄ΠΎΠ²Π°Π½ΠΈΡ ΡΠ²Π»ΡΠ΅ΡΡΡ ΠΎΡΠ³Π°Π½ΠΈΠ·Π°ΡΠΈΠΎΠ½Π½Π°Ρ ΠΊΡΠ»ΡΡΡΡΠ° Π² ΠΊΠΎΠΌΠΏΠ°Π½ΠΈΠΈ ΠΠΠ Β«ΠΠ°ΡΡΡ β Π’ΠΎΠΌΡΠΊ. Π¦Π΅Π»Ρ ΠΠΠ - ΡΠΎΡΡΠΎΠΈΡ Π² ΠΏΡΠ°ΠΊΡΠΈΡΠ΅ΡΠΊΠΎΠΉ ΡΠ°Π·ΡΠ°Π±ΠΎΡΠΊΠ΅ ΠΏΠΎ ΡΠΎΠ²Π΅ΡΡΠ΅Π½ΡΡΠ²ΠΎΠ²Π°Π½ΠΈΡ ΠΎΡΠ³Π°Π½ΠΈΠ·Π°ΡΠΈΠΎΠ½Π½ΠΎΠΉ ΠΊΡΠ»ΡΡΡΡΡ Π² ΠΊΠΎΠΌΠΏΠ°Π½ΠΈΠΈ ΠΠΠ Β«ΠΠ°ΡΡΡ β Π’ΠΎΠΌΡΠΊΒ». ΠΡΠ°ΠΊΡΠΈΡΠ΅ΡΠΊΠ°Ρ Π·Π½Π°ΡΠΈΠΌΠΎΡΡΡ ΡΠ°Π±ΠΎΡΡ Π·Π°ΠΊΠ»ΡΡΠ°Π΅ΡΡΡ Π² ΠΎΡΠ½ΠΎΠ²Π½ΡΡ
ΠΏΠΎΠ»ΠΎΠΆΠ΅Π½ΠΈΡΡ
ΠΈ Π²ΡΠ²ΠΎΠ΄Π°Ρ
ΠΈΡΡΠ»Π΅Π΄ΠΎΠ²Π°Π½ΠΈΡ Π΄ΠΎΠ²Π΅Π΄Π΅Π½Π½ΡΡ
Π΄ΠΎ ΡΡΠΎΠ²Π½Ρ ΠΊΠΎΠ½ΠΊΡΠ΅ΡΠ½ΡΡ
ΠΏΡΠ΅Π΄Π»ΠΎΠΆΠ΅Π½ΠΈΠΉ ΠΈ ΡΠ΅ΠΊΠΎΠΌΠ΅Π½Π΄Π°ΡΠΈΠΉ Π΄Π»Ρ ΠΊΠΎΠΌΠΏΠ°Π½ΠΈΠΈ. Π ΠΏΠ΅ΡΠ²ΠΎΠΉ Π³Π»Π°Π²Π΅ ΡΠ°ΡΡΠΌΠ°ΡΡΠΈΠ²Π°Π΅ΡΡΡ ΡΡΡΠ½ΠΎΡΡΡ ΠΎΡΠ³Π°Π½ΠΈΠ·Π°ΡΠΈΠΎΠ½Π½ΠΎΠΉ ΠΊΡΠ»ΡΡΡΡΡ, ΠΏΠΎΠ½ΡΡΠΈΠ΅ Β«ΠΎΡΠ³Π°Π½ΠΈΠ·Π°ΡΠΈΠΎΠ½Π½Π°Ρ ΠΊΡΠ»ΡΡΡΡΠ°Β», ΡΡΡΡΠΊΡΡΡΠ°, Π΄ΠΈΠ½Π°ΠΌΠΈΠΊΠ°, ΡΡΠ½ΠΊΡΠΈΠΈ ΠΈ ΡΠΈΠΏΡ ΠΎΡΠ³Π°Π½ΠΈΠ·Π°ΡΠΈΠΎΠ½Π½ΠΎΠΉ ΠΊΡΠ»ΡΡΡΡΡ. ΠΠΎ Π²ΡΠΎΡΠΎΠΉ Π³Π»Π°Π²Π΅ ΠΏΡΠΈΠ²ΠΎΠ΄ΠΈΡΡΡ ΠΎΠ±ΡΠ°Ρ Ρ
Π°ΡΠ°ΠΊΡΠ΅ΡΠΈΡΡΠΈΠΊΠ° ΠΊΠΎΠΌΠΏΠ°Π½ΠΈΠΈ, ΠΈΡΡΠ»Π΅Π΄ΡΠ΅ΡΡΡ Π±ΡΡΡΡΡΠ°Ρ ΠΊΡΠ»ΡΡΡΡΠ°, ΠΎΠΏΡΠ΅Π΄Π΅Π»ΡΠ΅ΡΡΡ Π΅Π΅ ΠΆΠ΅Π»Π°Π΅ΠΌΠΎΠ΅ ΡΠΎΡΡΠΎΡΠ½ΠΈΠ΅ ΠΈ ΠΏΡΠΎΠ²ΠΎΠ΄ΠΈΡΡΡ ΡΠ°Π·ΡΠ°Π±ΠΎΡΠΊΠ° ΠΏΠΎ ΡΠΎΠ²Π΅ΡΡΠ΅Π½ΡΡΠ²ΠΎΠ²Π°Π½ΠΈΡ ΠΎΡΠ³Π°Π½ΠΈΠ·Π°ΡΠΈΠΎΠ½Π½ΠΎΠΉ ΠΊΡΠ»ΡΡΡΡΡ Π² ΠΊΠΎΠΌΠΏΠ°Π½ΠΈΠΈ ΠΠΠ Β«ΠΠ°ΡΡΡ β Π’ΠΎΠΌΡΠΊΒ».
ΠΠ΅ΡΠΎΠ΄Ρ: ΡΠΌΠΏΠΈΡΠΈΡΠ΅ΡΠΊΠΈΠ΅ ΠΌΠ΅ΡΠΎΠ΄Ρ, Π°Π½ΠΊΠ΅ΡΠΈΡΠΎΠ²Π°Π½ΠΈΠ΅, ΡΠ΅ΠΎΡΠ΅ΡΠΈΡΠ΅ΡΠΊΠΈΠ΅ ΠΌΠ΅ΡΠΎΠ΄Ρ, Π°Π½Π°Π»ΠΈΠ· Π»ΠΈΡΠ΅ΡΠ°ΡΡΡΡ. ΠΠΎΠ²ΠΈΠ·Π½Π° ΠΈ ΠΏΡΠ°ΠΊΡΠΈΡΠ΅ΡΠΊΠ°Ρ Π·Π½Π°ΡΠΈΠΌΠΎΡΡΡ ΡΠ°Π±ΠΎΡΡ: ΠΠΎΠ²ΠΈΠ·Π½Π° Π΄Π°Π½Π½ΠΎΠΉ ΡΠ°Π±ΠΎΡΡ ΡΠΎΡΡΠΎΠΈΡ Π² ΡΠΎΠΌ, ΡΡΠΎ Π² ΡΠ΅Π·ΡΠ»ΡΡΠ°ΡΠ΅ ΠΏΡΠΎΠ΄Π΅Π»Π°Π½Π½ΠΎΠΉ ΡΠ°Π±ΠΎΡΡ Π±ΡΠ»ΠΈ Π½Π°ΠΉΠ΄Π΅Π½Ρ ΠΏΡΠ°ΠΊΡΠΈΡΠ΅ΡΠΊΠΈΠ΅ ΠΏΠΎΠ΄Ρ
ΠΎΠ΄Ρ Π² ΡΠ°Π·ΡΠ°Π±ΠΎΡΠΊΠ΅ ΡΠΎΠ²Π΅ΡΡΠ΅Π½ΡΡΠ²ΠΎΠ²Π°Π½ΠΈΡ ΠΊΡΠ»ΡΡΡΡΡ. ΠΡΠ°ΠΊΡΠΈΡΠ΅ΡΠΊΠ°Ρ Π·Π½Π°ΡΠΈΠΌΠΎΡΡΡ Π΄ΠΈΠΏΠ»ΠΎΠΌΠ½ΠΎΠΉ ΡΠ°Π±ΠΎΡΡ Π·Π°ΠΊΠ»ΡΡΠ°Π΅ΡΡΡ Π² Π²ΠΎΠ·ΠΌΠΎΠΆΠ½ΠΎΡΡΠΈ ΡΠ΅Π°Π»ΡΠ½ΠΎΠ³ΠΎ ΠΈΡΠΏΠΎΠ»ΡΠ·ΠΎΠ²Π°Π½ΠΈΡ ΠΏΡΠ΅Π΄Π»ΠΎΠΆΠ΅Π½Π½ΡΡ
ΠΈΠ½ΡΡΡΡΠΌΠ΅Π½ΡΠΎΠ² Π΄Π»Ρ ΠΊΠΎΠΌΠΏΠ°Π½ΠΈΠΈ ΠΠΠ Β«ΠΠ°ΡΡΡ β Π’ΠΎΠΌΡΠΊΒ».The problem of forming of organizational culture one of the most significant in the company, because of the clear structure of the organizational culture depends not only favorable existence in the organization, improving the professionalism and creativity of employees, but the final result of the activities of the company. The object of research is the company "Parus β Tomsk". The subject of research is organizational culture in the company "Sail β Tomsk. The purpose of the WRC is a practical design to improve the organizational culture of the company OOO "Parus β Tomsk". The practical significance of the work lies in the substantive provisions and conclusions of the study brought to the level of specific proposals and recommendations for the company. The first Chapter examines the nature of organizational culture, "organizational culture," structure, dynamics, functions and types of organizational culture. The second Chapter provides a General description of the company, examines the prevailing culture is determined by its desired state, and development is performed to improve the organizational culture of the company OOO "Parus β Tomsk".
Methods: empirical methods, survey, theoretical methods, analysis of the literature. The novelty and practical significance of the work: the Novelty of this work lies in the fact that the result of this work have been found practical approaches in developing the improvement culture. The practical significance of the thesis lies in the possibility of real use of the proposed tools for the company OOO "Parus β Tomsk"
Synthesis of magnetite nanoparticles by the method of co-precipitation and study of the influence of the reaction medium on their magnetic properties
Magnetite nanoparticles were obtained using the co-precipitation method under various synthesis conditions. The phase composition was investigated using X-ray diffraction analysis. The saturation magnetization of the obtained magnetic nanoparticles was investigated using vibrating-sample magnetometer. As a result, the samples obtained in a nitrogen atmosphere reveal a higher saturation magnetization value than the ones obtained in air
Gasgenese und Gasspeicherung im flΓΆzfΓΌhrenden Oberkarbon des Ruhr-Beckens
The present study investigates the generation, accumulation and occurrence of coalbedmethane (CBM) in the Ruhr Basin. It was triggered by a commercial CBM project performedjointly by DEUTSCHE STEINKOHLE AG (formerly RUHRKOHLE AG), RUHRGAs AG andCONOCO MINERALOEL GmbH. The aim of the project was to explore the CBM potential ofUpper Carboniferous strata and to evaluate the commercial producibility of CBM from suchreservoirs. This study provides a knowledge-based exploration model to delineate areas withpotentially high gas content. It also provides data for a more reliable quantification of suchreservoirs already at an early stage of exploration, prior to costly drilling operations.In order to quantify the gas generation potential in the Upper Carboniferous the amount oforganic matter both in coal seams and in dispersed form was estimated (214m/marea). Boththe maximum net coal thickness and the highest accumulation of dispersed organic matter(210 kg/m) occur in the Westphalian B 1. The total quantity of organic matter in thesediments of the Ruhr Basin (10.000 km) amounts to approximately 2.410 t. According to amass-balanced gas generation model one ton of terrestrial organic matter generates, within amaturity interval of 0.65 to 2.7 %VR, approximately 153 m methane, 81m carbon dioxideand 5 m nitrogen (STP). When applied to the amount and maturity of the organic matter inthe Ruhr Basin this corresponds to a total gas generation of 17.600 m/m. The UpperWestphalian A2 has been the most productive stratigraphic interval (10.4 m/m). Theportion of methane in the cumulative gas liberated from the organic matter rises withincreasing depth and maturity of the organic matter to a maximum of 65 Vol.% in Namur Ccoals. Also, gas generation from terrestrial OM was studied both by means of non-isothermalopen-system pyrolysis and - for the first time - by on-line Pyrolysis-GC-IRMS. For fivepyrolysis products studied with this method the experiments illustrate a strong isotopefractionation and local isotopic maxima and minima.The gas storage in coal seams was studied using a newly designed high pressure/hightemperature adsorption device. The data of more than fifty experiments at pressures of up to20 MPa and maximum temperatures of 175 Β°C showed an increase of adsorption capacitywith increasing pressure, and decreasing temperature and moisture content. Measurements ofthe specific surface area (CO) gave highest values for vitrain (vitrinite-rich samples).Generally, smaller-than-average surface areas were observed within a maturity range of 1.0 to1.4 %VR. Based on the experimental data correlations were established that can be used tomodel the depth dependence of the adsorption capacity of the organic matter. The proposeddynamic sorption model links experimental results to the geological evolution of sedimentarybasins by relating phases of tectonic uplift and subsidence to adsorption/desorption events atdifferent depth intervals. Thus, the model provides a new interpretation for the accumulationand regional distribution of CBM reservoirs in the context basin evolution.The occurrence of CBM in the Ruhr Basin was examined both in a thorough geochemical andisotopic study of two exploration wells and also by evaluating exploration data of the local [...
Gasgenese und Gasspeicherung im flΓΆzfΓΌhrenden Oberkarbon des Ruhr-Beckens
The present study investigates the generation, accumulation and occurrence of coalbedmethane (CBM) in the Ruhr Basin. It was triggered by a commercial CBM project performedjointly by DEUTSCHE STEINKOHLE AG (formerly RUHRKOHLE AG), RUHRGAs AG andCONOCO MINERALOEL GmbH. The aim of the project was to explore the CBM potential ofUpper Carboniferous strata and to evaluate the commercial producibility of CBM from suchreservoirs. This study provides a knowledge-based exploration model to delineate areas withpotentially high gas content. It also provides data for a more reliable quantification of suchreservoirs already at an early stage of exploration, prior to costly drilling operations.In order to quantify the gas generation potential in the Upper Carboniferous the amount oforganic matter both in coal seams and in dispersed form was estimated (214m/marea). Boththe maximum net coal thickness and the highest accumulation of dispersed organic matter(210 kg/m) occur in the Westphalian B 1. The total quantity of organic matter in thesediments of the Ruhr Basin (10.000 km) amounts to approximately 2.410 t. According to amass-balanced gas generation model one ton of terrestrial organic matter generates, within amaturity interval of 0.65 to 2.7 %VR, approximately 153 m methane, 81m carbon dioxideand 5 m nitrogen (STP). When applied to the amount and maturity of the organic matter inthe Ruhr Basin this corresponds to a total gas generation of 17.600 m/m. The UpperWestphalian A2 has been the most productive stratigraphic interval (10.4 m/m). Theportion of methane in the cumulative gas liberated from the organic matter rises withincreasing depth and maturity of the organic matter to a maximum of 65 Vol.% in Namur Ccoals. Also, gas generation from terrestrial OM was studied both by means of non-isothermalopen-system pyrolysis and - for the first time - by on-line Pyrolysis-GC-IRMS. For fivepyrolysis products studied with this method the experiments illustrate a strong isotopefractionation and local isotopic maxima and minima.The gas storage in coal seams was studied using a newly designed high pressure/hightemperature adsorption device. The data of more than fifty experiments at pressures of up to20 MPa and maximum temperatures of 175 Β°C showed an increase of adsorption capacitywith increasing pressure, and decreasing temperature and moisture content. Measurements ofthe specific surface area (CO) gave highest values for vitrain (vitrinite-rich samples).Generally, smaller-than-average surface areas were observed within a maturity range of 1.0 to1.4 %VR. Based on the experimental data correlations were established that can be used tomodel the depth dependence of the adsorption capacity of the organic matter. The proposeddynamic sorption model links experimental results to the geological evolution of sedimentarybasins by relating phases of tectonic uplift and subsidence to adsorption/desorption events atdifferent depth intervals. Thus, the model provides a new interpretation for the accumulationand regional distribution of CBM reservoirs in the context basin evolution.The occurrence of CBM in the Ruhr Basin was examined both in a thorough geochemical andisotopic study of two exploration wells and also by evaluating exploration data of the local [...