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Journal articles on the topic "Thesis Aero 1993 M.S"

1

Nechaev, Igor V., та Alexander V. Vvedenskii. "Квантово-химическое моделирование взаимодействия в системе MeN(H2O)M (Me = Cu, AgG, Au; N = 1-3; M = 1, 2)". Kondensirovannye sredy i mezhfaznye granitsy = Condensed Matter and Interphases 21, № 1 (2019): 105–15. http://dx.doi.org/10.17308/kcmf.2019.21/722.

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Моделирование реакции малых кластеров IB металлов с молекулами воды проведено в рамках теории функционала плотности. Рассчитана структура, колебательные частоты, зарядовое распределение и другие характеристики изомеров Men(H2O)m (Me = Cu, Ag, Au; n = 1-3; m = 1, 2). Показано, что частицы Cu2 и Cu3 термодинамически способны разлагать воду на водород и гидроксил при стандартных условиях, другие рассмотренные кластеры IB металлов подобной активностью не обладают.
 
 
 ЛИТЕРАТУРА
 
 Vigdorovich V. , Tsygankova L. E. , Shel’ N. V. Protection of Metals and Physical Chemistry of Surfaces, 2015, vol. 51, no. 4, pp. 567-574. https://doi.org/10.1134/s2070205115040346 
 de Heer W. A. Mod. Phys., 1993, vol. 65, pp. 611. https://doi.org/10.1103/revmodphys.65.611
 Serebrennikov L. V., Davlyatshin D. I., Golovkin A. V. Russian Journal of Pphysical Chemistry A, 2010, vol. 84, pp. 2082. https://doi.org/10.1134/s0036024410120137
 Tretyakov Y. D., Goodilin E. A. Russian Chemical Reviews, 2009, vol. 78, pp. 801. https://doi.org/10.1070/rc2009v078n09abeh004029
 Melikhov V. I. Herald of the Russian Academy of Sciences, 2007, vol. 77, pp. 563-567. https://doi.org/10.1134/s1019331607060032
 Valden M., Lai X., Goodman W. Science, 1998, vol. 281, pp. 1647. https://doi.org/10.1126/science.281.5383.1647
 Park A. Thesis Ph.D. Rice University, 1988, pp. 126-160.
 Eachus R. S., Marchetti A. P., Muenter A. A. Rev. Phys. Chem., 1999, vol. 50, pp. 117. https://doi.org/10.1146/annurev.physchem.50.1.117
 Elghanian R., Srorhoff J. J., Mucic R. C., et al. Science, 1997, vol. 277, pp. 1078. https://doi.org/10.1126/science.277.5329.1078
 Doroshenko A. A., Nechaev I. V., Vvedenskii A. V. Russian Journal of Physical Chemistry A, 2014, vol. 88, pp. 1542. https://doi.org/10.1134/s003602441409012x
 Moskovits M. Mod. Phys., 1985, vol. 57, pp. 783. https://doi.org/10.1103/revmodphys.57.783
 Adamo C., Scuseria G.E., Barone V. Chem. Phys., 1999, vol. 111, pp. 2889. https://doi.org/10.1063/1.479571
 Dunning Jr. T. H. Chem. Phys., 1989, vol. 90, pp. 1007. https://doi.org/10.1063/1.456153
 Stoll H., Fuentealba P., Schwerdtfeger P., et al. Chem. Phys., 1984, vol. 81, pp. 2732. DOI: 10.1063/1.447992
 Reed A. E, Kurtiss L. A., Weinhold F. Rev., 1988, vol. 88, pp. 899. DOI: 10.1021/cr00088a005
 Frisch M. J., Trucks G. W., Schlegel H. B., et al. Gaussian 09 Revision D.01. Gaussian Inc., Wallingford CT, 2009.
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 Merrick J. P., Moran D., Radom L. Phys. Chem. A., 2007, vol. 111, pp. 11683. DOI: 10.1021/jp073974n
 Barone V. Chem. Phys., 2004, vol. 120, pp. 3059. DOI: 10.1063/1.1637580
 Molecular Constants of Inorganic Compounds / Ed. by K.S Krasnova. Leningrad, Chemistry Publ., 1979, 448 p. (in Russ.)
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Thanh, Nguyen Trung, Paul Jing Liu, Mai Duc Dong, et al. "Late Pleistocene-Holocene sequence stratigraphy of the subaqueous Red River delta and the adjacent shelf." VIETNAM JOURNAL OF EARTH SCIENCES 40, no. 3 (2018): 271–87. http://dx.doi.org/10.15625/0866-7187/40/3/12618.

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The model of Late Pleistocene-Holocene sequence stratigraphy of the subaqueous Red River delta and the adjacent shelf is proposed by interpretation of high-resolution seismic documents and comparison with previous research results on Holocene sedimentary evolution on the delta plain. Four units (U1, U2, U3, and U4) and four sequence stratigraphic surfaces (SB1, TS, TRS and MFS) were determined. The formation of these units and surfaces is related to the global sea-level change in Late Pleistocene-Holocene. SB1, defined as the sequence boundary, was generated by subaerial processes during the Late Pleistocene regression and could be remolded partially or significantly by transgressive ravinement processes subsequently. The basal unit U1 (fluvial formations) within incised valleys is arranged into the lowstand systems tract (LST) formed in the early slow sea-level rise ~19-14.5 cal.kyr BP, the U2 unit is arranged into the early transgressive systems tract (E-TST) deposited mainly within incised-valleys under the tide-influenced river to estuarine conditions in the rapid sea-level rise ~14.5-9 cal.kyr BP, the U3 unit is arranged into the late transgressive systems tract (L-TST) deposited widely on the continental shelf in the fully marine condition during the late sea-level rise ~9-7 cal.kyr BP, and the U4 unit represents for the highstand systems tract (HST) with clinoform structure surrounding the modern delta coast, extending to the water depth of 25-30 m, developed by sediments from the Red River system in ~3-0 cal.kyr BP.ReferencesBadley M.E., 1985. Practical Seismic Interpretation. International Human Resources Development Corporation, Boston, 266p.Bergh G.D. V.D., Van Weering T.C.E., Boels J.F., Duc D.M, Nhuan M.T, 2007. Acoustical facies analysis at the Ba Lat delta front (Red River delta, North Vietnam. Journal of Asian Earth Science, 29, 532-544.Boyd R., Dalrymple R., Zaitlin B.A., 1992. Classification of Elastic Coastal Depositional Environments. Sedimentary Geology, 80, 139-150.Catuneanu O., 2002. Sequence stratigraphy of clastic systems: concepts, merits, and pitfalls. Journal of African Earth Sciences, 35, 1-43.Catuneanu O., 2006. Principles of Sequence Stratigraphy. Elsevier, Amsterdam, 375p.Catuneanu O., Abreu V., Bhattacharya J.P., Blum M.D., Dalrymple R.W., Eriksson P.G., Fielding C.R., Fisher W.L., Galloway W.E., Gibling M.R., Giles K.A., Holbrook J.M., Jordan R., Kendall C.G. St. C., Macurda B., Martinsen O.J., Miall A.D., Neal J.E., Nummedal D., Pomar L., Posamentier H.W., Pratt B.R., Sarg J.F., Shanley K.W., Steel R. J., Strasser A., Tucker M.E., Winker C., 2009. Towards the standardization of sequence stratigraphy. Earth-Science Reviews, 92, 1-33.Catuneanu O., Galloway W.E., Kendall C.G. St C., Miall A.D., Posamentier H.W., Strasser A. and Tucker M.. E., 2011. Sequence Stratigraphy: Methodology and Nomenclature. Newsletters on Stratigraphy, 44(3), 173-245.Coleman J.M and Wright L.D., 1975. Modern river deltas: variability of processes and sand bodies. In: Broussard M.L (Ed), Deltas: Models for exploration. Houston Geological Society, Houston, 99-149.Doan Dinh Lam, 2003. History of Holocene sedimentary evolution of the Red River delta. PhD thesis in Vietnam, 129p (in Vietnamese).Duc D.M., Nhuan M.T, Ngoi C.V., Nghi T., Tien D.M., Weering J.C.E., Bergh G.D., 2007. Sediment distribution and transport at the nearshore zone of the Red River delta, Northern Vietnam. Journal of Asian Earth Sciences, 29, 558-565.Dung B.V., Stattegger K., Unverricht D., Phach P.V., Nguyen T.T., 2013. Late Pleistocene-Holocene seismic stratigraphy of the Southeast Vietnam Shelf. Global and Planetary Change, 110, 156-169.Embry A.F and Johannessen E.P., 1992. T-R sequence stratigraphy, facies analysis and reservoir distribution in the uppermost Triassic-Lower Jurassic succession, western Sverdrup Basin, Arctic Canada. In: Vorren T.O., Bergsager E., Dahl-Stamnes O.A., Holter E., Johansen B., Lie E., Lund T.B. (Eds.), Arctic Geology and Petroleum Potential. Special Publication. Norwegian Petroleum Society (NPF), 2, 121-146.Funabiki A., Haruyama S., Quy N.V., Hai P.V., Thai D.H., 2007. Holocene delta plain development in the Song Hong (Red River) delta, Vietnam. Journal of Asian Earth Sciences, 30, 518-529.General Department of Land Administration., 1996. Vietnam National Atlas. General Department of Land Administration, Hanoi, 163p.Hanebuth T.J.J. and Stattegger K., 2004. Depositional sequences on a late Pleistocene-Holocene tropical siliciclastic shelf (Sunda shelf, Southeast Asia). Journal of Asian Earth Sciences, 23, 113-126.Hanebuth T.J.J., Voris H.K.., Yokoyama Y., Saito Y., Okuno J., 2011. Formation and fate of sedimentary depocenteres on Southeast Asia’s Sunda Shelf over the past sea-level cycle and biogeographic implications. Eath-Science Reviews, 104, 92-110.Hanebuth T., Stattegger K and Grootes P. M., 2000. Rapid flooding of the Sunda Shelf: a late-glacial sea-level record. Science, 288, 1033-1035.Helland-Hansen W and Gjelberg, J.G., 1994. Conceptual basis and variability in sequence stratigraphy: a different perspective. Sedimentary Geology, 92, 31-52.Hori K., Tanabe S., Saito Y., Haruyama S., Nguyen V., Kitamura., 2004. Delta initiation and Holocene sea-level change: example from the Song Hong (Red River) delta, Vietnam. Sedimentary Geology, 164, 237-249.Hunt D. and Tucker M.E., 1992. Stranded parasequences and the forced regressive wedge systems tract: deposition during base-level fall. Sedimentology Geology, 81, 1-9.Hunt D. and Tucker M.E., 1995. Stranded parasequences and the forced regressive wedge systems tract: deposition during base-level fall-reply. Sedimentary Geology, 95, 147-160.Lam D.D. and Boyd W.E., 2000. Holocene coastal stratigraphy and model for the sedimentary development of the Hai Phong area in the Red River delta, north Vietnam. Journal of Geology (Series B), 15-16, 18-28.Lieu N.T.H., 2006. Holocene evolution of the Central Red River Delta, Northern Vietnam. PhD thesis of lithological and mineralogical in Germany, 130p.Luu T.N.M., Garnier J., Billen G., Orange D., Némery J., Le T.P.Q., Tran H.T., Le L.A., 2010. Hydrological regime and water budget of the Red River Delta (Northern Vietnam). Journal of Asian Earth Sciences, 37, 219-228.Mather S.J., Davies J., Mc Donal A., Zalasiewicz J.A., and Marsh S., 1996. The Red River Delta of Vietnam. British Geological Survey Technical Report WC/96/02, 41p.Mathers S.J. and Zalasiewicz J.A.,1999. Holocene sedimentary architecture of the Red River delta, Vietnam. Journal of Coastal Research, 15, 314-325.Milliman J.D. and Mead R.H., 1983. Worldwide delivery of river sediment to the oceans. Journal of Geology, 91, 1-21.Milliman J.D and Syvitski J.P.M., 1992. Geomorphic/tectonic control of sediment discharge to the Ocean: the importance of small mountainous rivers. Journal of Geology, 100, 525-544.Mitchum Jr. R.M., Vail P.R., 1977. Seismic stratigraphy and global changes of sea-level. Part 7: stratigraphic interpretation of seismic reflection patterns in depositional sequences. In: Payton C.E. (Ed.), Seismic Stratigraphy-Applications to Hydrocarbon Exploration, A.A.P.G. Memoir, 26, 135-144.Nguyen T.T., 2017. Late Pleistocene-Holocene sedimentary evolution of the South East Vietnam Shelf, PhD thesis (in Vietnamese), Hanoi University of Science, Vietnam, 169p.Nummedal D., Riley G.W., Templet P.T., 1993. High-resolution sequence architecture: a chronostratigraphic model based on equilibrium profile studies. In: Posamentier H.W., Summerhayes C.P., Haq B.U., Allen G.P. (Eds.), Sequence stratigraphy and Facies Associations. International Association of Sedimentologists Special Publication, 18, 55-58.Posamentier H.W. and Allen G.P., 1999. Siliciclastic sequence stratigraphy: concepts and applications. SEPM Concepts in Sedimentology and Paleontology, 7, 210p.Posamentier H.W., Jervey M.T. and Vail P.R., 1988. Eustatic controls on clastic deposition I-Conceptual framework. Sea-level changes-An Integrated Approach, The Society of Economic Paleontologists and Mineralogist. SEPM Special Publication, 42, 109-124.Reineck H.E., Singh I.B., 1980. Depositional sedimentary environments with reference to terrigenous clastics. Springer-Verlag Berlin Heidelberg New York, 551p. Ross K., 2011. Fate of Red River Sediment in the Gulf of Tonkin, Vietnam. Master Thesis. North Carolina State University, 91p.Saito Y., Katayama H., Ikehara K., Kato Y., Matsumoto E., Oguri K., Oda M., Yumoto M. 1998. Transgressive and highstand systems tracts and post-glacial transgression, the East China Sea. Sedimentary Geology, 122, 217-232.Stattegger K., Tjallingii R., Saito Y., Michelli M., Nguyen T.T., Wetzel A., 2013. Mid to late Holocene sea-level reconstruction of Southeast Vietnam using beachrock and beach-ridge deposits. Global and Planetary Change, 110, 214-222.Tanabe S., Hori K., Saito Y., Haruyama S., Doanh L.Q., Sato Y., Hiraide S., 2003a. Sedimentary facies and radiocarbon dates of the Nam Dinh-1 core from the Song Hong (Red River) delta, Vietnam. Journal of Asian Earth Sciences, 21, 503-513.Tanabe S., Hori K., Saito Y., Haruyama S., Phai V.V., Kitamura A., 2003b. Song Hong (Red River) delta evolution related to millennium-scale Holocene sea-level changes. Quaternary Science Reviews, 22(21-22), 2345-2361.Tanabe S., Saito Y., Lan V.Q., Hanebuth T.J.J., Lan N.Q., Kitamura A., 2006. Holocene evolution of the Song Hong (Red River) delta system, northern Vietnam. Sedimentary Geology, 187, 29-61.Thanh T.D. and Huy D.V., 2000. Coastal development of the modern Red River Delta. Bulletin of the Geological Survey of Japan, 5, 276.Tjallingii R., Stattegger K., Wetzel A., Phung VP., 2010. Infilling and flooding of the Mekong River incised valley during deglacial sea-level rise. Quaternary Science Reviews, 29, 1432-1444.Vail P.R., 1987. Seismic stratigraphy interpretation procedure. In: Bally, A.W. (Ed), Atlats of Seismic Stratigraphy. American Association of Petroleum Geologist Studies in Geology, 27, 1-10.Van Wagoner J.C., Posamentier H.W., Mitchum R.M., Vail P.R., Sarg P.R., Louit J.F., Hardenbol J., 1988. An overview of the fundamental of sequence stratigraphy and key definitions. An Integrated Approach, SEPM Special Publication, 42, 39-45.Veeken P.C.H., 2006. Seismic stratigraphy Basin Analysis and Reservoir Characterization. Handbook of geophysical exploration, Elsevier, Oxford, 37509p.Yoo D.G., Kim S.P., Chang T.S., Kong G.S., Kang N.K., Kwon Y.K., Nam S.L., Park S.C., 2014. Late Quaternary inner shelf deposits in response to late Pleistocene-Holocene sea-level changes: Nakdong River, SE Korea. Quaternary International, 344, 156-169.
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Rzaguliyev, Vidadi A., Oruj S. Kerimli, Dilbar S. Ajdarova, Sharafat H. Mammadov та Ozbek M. Aliev. "Фазовые равновесия в системах Ag8SnS6–Cu2SnS3 и Ag2SnS3–Cu2Sn4S9". Kondensirovannye sredy i mezhfaznye granitsy = Condensed Matter and Interphases 21, № 4 (2019): 544–51. http://dx.doi.org/10.17308/kcmf.2019.21/2365.

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Комплексными методами физико-химического анализа (дифференциально-термический, рентгенофазовый, микроструктурный, измерение микротвердости и определение плотности) изучены фазовые равновесия и построены Т–х фазовые диаграммыв системах Ag8SnS6–Cu2SnS3 и Ag2SnS3–Cu2Sn4S9. Показано, что система Ag8SnS6–Cu2SnS3является квазибинарным сечением квазитройной системы Ag2S-SnS2-Cu2S и относится кпростому эвтектическому типу с ограниченными областями растворимости на основеисходных сульфидов. Координаты эвтектической точки: 50 mol % Ag2SnS3 И Т = 900 К.Растворимость на основе Ag8SnS6 и Cu2SnS3 при эвтектической температуре простираетсядо 20 и 28 mol % соответственно. С уменьшением температуры твердые растворы распадаются и при 300 К составляют 5 и 10 mol %. Установлено, что с увеличением концентрацииAg8SnS6 в твердых растворах (Cu2SnS3)1-х (Ag8SnS6)х параметр кубической решетки увеличивается от а = 0.5445 nm (для чистого Cu2SnS3) до а = 0.725 nm (для состава х = 0.1) т. е. концентрационная зависимость параметра решетки имеет линейный характер.Система Ag2SnS3–Cu2Sn4S9 из-за перитектического плавления Cu2Sn4S9 имеет сложный характер и является частично квазибинарным сечением. Квазибинарность нарушается вобласти концентрации 65-100 mol % Cu2Sn4S9 и выше температуры 900 К. Твердые растворына основе Ag2SnS3 и Cu2Sn4S9 узкие и при 300 К составляют 10; 2.5 mol % соответственно
 
 
 
 
 ЛИТЕРАТУРА1. Wang N., Fan A. K. An experimental study of the Ag2S-SnS2 pseudobinary join // Neues Jahrb. Mineral.-Abh, 1989, v. 160, pp. 33–36.2. Wang N. New data for Ag8SnS6 (canfeildite) and Ag8GeS6 (argyrodite) // Neues Jahrb. Mineral. Monatsh.,1978, pp. 269–272.3. Бабанлы М. Б., Юсибов Ю. А., Абишев В. Т. Трехкомпонентные халькогениды на основе медии серебра. Баку: Изд-во БГУ, 1993, 342 с.4. Parasyuk O. V., Chykhrij S. I., Bozhko V. V., Piskach L. V., Bogdanyuk M. S., Olekseyuk I. D.,Bulatetska L. V., Pekhnyo. Phase diagramm of the Ag2S–HgS–SnS2 system and single crystal prepartion,crystal structure and properties of Ag2HgSnS4 // J. Alloys and Compounds, 2005, v. 399, pp. 32–37. DOI: https://doi.org/10.1016/j.jallcom.2005.03.0085. Olekseyuk I. D., Dudchak I. B., Piskach L. V. Phase equilibria in the Cu2S–ZnSe–SnS2 // J. Alloys andCompounds, 2004, v. 368, pp. 135–143. https:doi.org/10.1016/j.jallcom.2003.08.0846. Ollitrault-Fitchet R., Rivet J., Flahaut J., et.al. Description du systeme ternaire Ag–Sn–Se // J. Less-Common. Met., 1988, v. 138(2), pp. 241–261. DOI:https://doi.org/10.1016/0022-5088(88)90113-07. Delgado C. E., Mora A. J., Marcano E. Crystal structure refi nement of the semiconducting compoundCu2SnSe3 from X-ray powder difraction data // Mater. Res. Bull., 2003, v. 38, pp. 1949–1955. DOI: https://doi.org/10.1016/j.materresbull.2003.09.0178. Parasyuk O. V., Olekseyuk I. D., Marchuk O. V. The Cu2Se–HgSe–SnSe2 // J. Alloys and Compounds.,1999, v. 287, pp. 197–205. DOI: https//doi.org/10.1016/S0925-8388(99)00047-X9. Parasyuk O. V., Gulay L. D., Piskach L. V., Kumanska Yu. O. The Ag2Se–HgSe–SnSe2 system and thecrystal structure of the Ag2HgSnSe4 // J. Alloys and Сompounds, 2002, v. 339, pp.1 40–143. DOI: https//doi.org/10.1016/S0925-8388(01)01985-510. Babanly M. B., Yusibov Y. A., Babanly N. B. Electromotive force and measucement in several systema.Ed. by S. Kara, Intechneb. Org., 2011, pp. 57–58.11. Gulay L. D., Olekseyuk I. D., Parasyuk O. V. Crystal structure of b-Ag8SnSe6 // J. Alloys and compounds,2002, v. 339, pp. 113–117. DOI: https//doi.org/10.1016/S0925-8388(01)01970-312. Гусейнов Г. М. Получение соединения Ag8SnS6 в среде диметилформамида // Вестн. Томского гос. ун-та. Химия, 2016, № 1(3), c. 24–34. Режим доступа: fi le:///C:/Users/Lab351/Downloads/sub_%20%20in%20dimethylformamide%20medium.pdf (дата обращения: 19.09.2019)13. Gorchov O. Les composes Ag8MX6 (M = Si, Ge, Sn et X = S, Se, Te) // Bull. Soc. Chim. Fr., 1968, № 6.pp. 2263–2275.14. Kokhan O. P. The Interactions in Ag2X–BIVX2 (BIV – Si, Ge, Sn; X – S, Se) systems and the propertiesof compounds. Doctoral Thesis, Uzhgorod, Uzhgorod State Univ., 1996.15. Onoda U., Chen X. A., Sato A., Wada H. Crystal structure and twinning of monoclinic Cu2SnS3 // Mater.Res. Bull., 2000, v. 35, № 8, pp. 1563–1570. DOI: https//doi.org/10.1016/S0025-5408(00)00347-016. Рзагулиев В. А., Керимли О. Ш., Мамедов Ш. Г. Изучение квазитройной системы Ag2S–SnS2–Cu2S по разрезу Ag8SnS6–Cu2SnS3. Труды Международ. научно–практич. конф., Россия, Белгород,2019, c. 18.17. Рзагулиев В. А., Керимли О. Ш., Маме дов Ш. Г. Исследование квазибинарного разреза Cu2SnS3–Ag2SnS3 в квазитройной системеAg2S–Cu2S–SnS2 . Труды XXI Междун. конф., Санкт-Петербург, 2019,c. 20–21.18. Цигика В. В., Переш Е. Ю., Лазарев В. В. и др. Получение и свойства мнонокристаллов соединений/TlPbJ3, Tl3PbJ5, TlSnJ3, TlSn2J5 and Tl3PbBr5 Изв. АН СССР. Неорган. материалы, 1981, т. 17(6), c. 970–974.
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Perrin, Yves. "La maison de M. Lucretius Fronto, ou les difficultés de la connaissance des IIIeme et IVeme styles pompéiens - W. J. Th. PETERS con E. M. MOORMANN, T. L. HERES, H. BRUNSTING, S. L. WYNIA, LA CASA DI MARCUS LUCRETIUS FRONTO A POMPEI E LE SUE PITTURE (Scrinium V, Thesis Publishers, Amsterdam, 1993). Pp. 429, many figs. including colour. ISBN 90-5170-163-2. f 265,--." Journal of Roman Archaeology 11 (1998): 542–46. http://dx.doi.org/10.1017/s1047759400017608.

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Hung, Tran Trong, Tran Anh Tu, Dang Thuong Huyen, and Marc Desmet. "Presence of trace elements in sediment of Can Gio mangrove forest, Ho Chi Minh city, Vietnam." VIETNAM JOURNAL OF EARTH SCIENCES 41, no. 1 (2019): 21–35. http://dx.doi.org/10.15625/0866-7187/41/1/13543.

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Can Gio mangrove forest (CGM) is located downstream of Ho Chi Minh City (HCMC), situated between an estuarine system of Dong Nai - Sai Gon river and a part of Vam Co river. The CGM is the largest restored mangrove forest in Vietnam and the UNESCO’s Mangrove Biosphere Reserve. The CGM has been gradually facing to numeric challenges of global climate change, environmental degradation and socio-economic development for the last decades. To evaluate sediment quality in the CGM, we collected 13 cores to analyze for sediment grain size, organic matter content, and trace element concentration of Cd, Cr, Cu, Ni, Pb, Zn. Results showed that trace element concentrations ranged from uncontaminated (Cd, Cu, and Zn) to very minor contaminated (Cr, Ni, and Pb). The concentrations were gradually influenced by suspended particle size and the mangrove plants.ReferencesAnh M.T., Chi D.H., Vinh N.N., Loan T.T., Triet L.M., Slootenb K.B.-V., Tarradellas J., 2003. Micropollutants in the sediment of Sai Gon – Dong Nai rivers: Situation and ecological risks. Chimia International Journal for Chemistry, 57, 09(0009–4293), 537–541.Baruddin N.A., Shazili N.A., Pradit S., 2017. Sequential extraction analysis of heavy metals in relation to bioaccumulation in mangroves, Rhizophora mucronata from Kelantan delta, Malaysia. AACL Bioflux, 10(2), 172-181. Retrieved from www.bioflux.com/aacl.Bravard J.-P., Goichot M., Tronchere H., 2014. An assessment of sediment transport processes in the lower Mekong river based on deposit grain size, the CM technique and flow energy data. Geomorphology, 207, 174-189.Cang L.T., Thanh N.C. 2008. Importing and exporting sediment to and from mangrove forest at Dong Trang estuary, Can Gio district, Ho Chi Minh city. Science & Technology Development, 11(04), 12-18.Carignan J., Hild P., Mevelle G., Morel J., Yeghicheyan D., 2001. 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Samry, Wannofri. "THE ROLE OF MASS MEDIA AND MINANGKABAU IDENTITY." Book Chapters of The 1st Jakarta International Conference on Social Sciences and Humanities (JICoSSH) 1 (January 25, 2019): 52–64. http://dx.doi.org/10.33822/jicossh.v1i1.1.

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Abstract:
Since early of twentieth century mass media is one of the professional jobs which they done By Minangkabau People, both as journalist or auhtor and publisher. Beside as teacher carier, It seems that the mass media is the professional field that done ealiest of them. Establishing of Minangkabau identity is closely ralated to existence of mass media; with mass media progressing and having dialectic. The intelectual richness of Minangkabau since the early 20th century was known at national level is also not separated from the existence of mass media. Their identity also determained by the mass media; locality, nationalism and globalization influences are processed in mass media to form different Minangkabau world from time to time. This paper presents the establishing of the identiy of Minangkabau people through the mass media on various problem in a historical perspective, mainly after 1950’s.
 
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Pacciolla, Aureliano. "EMPATHY IN TODAYS CLINICAL PSYCHOLOGY AND IN EDITH STEIN." Studia Philosophica et Theologica 18, no. 2 (2019): 138–60. http://dx.doi.org/10.35312/spet.v18i2.29.

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 By Stein Edith:
 
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 – Fenomenologia dell’essere umano – Lineamenti di una filosofia al femminile, Città Nuova, Roma 1992.
 – Analisi fenomenologica della volontà. Edmund Husserl ed Edith Stein, in «Per la filosofia», 1994, n. 31, pp. 24-29.
 – Lo studio dell’anima fra psicologia e fenomenologia in Edith Stein, in Sogno e mondo, Edizioni Scientifiche Italiane, Napoli 1995, pp. 7-25.
 – Edith Stein. Invito alla lettura, Edizioni San Paolo, Milano 1999.
 – Edith Stein, Piemme, Casale Monferrato 2000.
 – Empatia e dialogo: un’analisi fenomenologica, in A. DENTONE (a cura di), Dialogo, silenzio, empatia, Bastoni Editrice Italiana, Foggia 2000, pp. 65-85.
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 – Edith Stein: lo spirito umano in cammino verso la santità in D’Ambra, Michele(a cura di), Edith Stein.Lo Spirito e la santità, «Quaderni dell’AIES», n. 2, Edizioni OCD, Roma 2007.
 Alfossi, Maura. et al., Guarire o curare? Comunicazione ed empatia in medicina, La Meridiana, Molfetta (BA), 2008.
 Balzer, Carmen, The Empathy Problem in Edith Stein, in Huusserlian Phenomenology in a New Key. Intersubjectivity, Ethos, the Social Sphere, Human Encouter, Pathos, ed. by A. T. Tymieniecka, Kluwe Academic Publisher, Dordrecht-Boston-London, in «AnalectaHusserliana», 35 (1991), pp. 271-278.
 Baron-Cohen, Simon., La scienza del male. L’empatia e le origini della crudeltà, Cortina, Milano, 2012.
 Bellingreri, Antonio, Per una pedagogia dell’empatia, Vita e Pensiero, Milano, 2005.
 Bettinelli, Carla,Il pensiero di Edith Stein. Dalla fenomenologia alla scienza della Croce, Vita e Pensiero, Milano 1976.
 – Il problema dell’Einfülung, in «Hermeneutica», 9 (1989), pp. 291-304.
 – La fenomenologia, uno sguardo sulla verità, in «Aquinas», 37 (1994), pp. 377-386.
 – L’itinerario di Edith Stein: dalla psicologia alla metafisica, alla mistica, in «Letture», 32 (1997), pp. 505-524.
 Boella, Laura and Buttarelli Annarosa,Per amore di altro. L’empatia a partire da Edith Stein, Raffaello Cortina Editore, Milano 2000.
 – Grammatica del sentire. Compassione, Simpatia, Empatia, CUEN, Milano, 2004.
 Bonino, Silvia, et al. (a cura di), Empatia. I processi di condivisione delle emozioni, Giunti, Firenze, 1998.
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 Cerri Musso, Renza,La pedagogia dell’Einfühlung. Saggio su Edith Stein, La Scuola, Brescia, 1955.
 Costantini, Elio,Einfühlung und Intersubjektivitätbei Edith Stein und bei Husserl, in The Great Chain of Being and Italian Phenomenology, in «AnalectaHusserliana»,, 11 (1981), pp. 335-339.
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 – Note sull’empatia nell’approccio interpersonale, in «Aquinas», 30 (1987), pp. 135-140.
 – L’empatia, conoscenza dell’”Io” estraneo, in «Studium», 86 (1990), pp. 73-91.
 D’Ambra, Michele,Il mistero e la persona nell’opera di Edith Stein, in «Aquinas», 34 (1997), pp. 581-591.
 D’Ippolito, Maria Bianca,L’analisi fenomenologica dell’anima, in«Aquinas», 41 (1997), pp. 61-67.
 De Waal Frans., L’età dell’empatia. Lezioni della natura per una società più solidale, Garzanti, Milano, 2011.
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Utomo, Muhajir, Irwan Sukri Banuwa, Henrie Buchari, Yunita Anggraini, and Berthiria. "Long-term Tillage and Nitrogen Fertilization Effects on Soil Properties and Crop Yields." JOURNAL OF TROPICAL SOILS 18, no. 2 (2013): 131. http://dx.doi.org/10.5400/jts.2013.v18i2.131-139.

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The impact of agricultural intensification on soil degradation now is occurring in tropical countries. The objective of this study was to determine the effect of long-term tillage and N fertilization on soil properties and crop yields in corn-soybean rotation. This long-term study which initiated since 1987 was carried out on a Typic Fragiudult soil at Politeknik Negeri Lampung, Sumatra (105o13’45.5"-105o13’48.0"E, 05o21’19.6"-05o21’19.7"S) in 2010 and 2011. A factorial experiment was arranged in a randomized block design with four replications. The first factor was tillage system namely intensive tillage (IT) and conservation tillage (CT) which consist of minimum tillage (MT) and no-tillage (NT); while the second factor was N fertilization with rates of 0, 100 and 200 kg N ha-1 applied for corn, and 0, 25, and 50 kg N ha-1 for soybean. The results showed that bulk density and soil strength at upper layer after 24 years of cropping were similar among treatments, but the soil strength under IT at 50-60 cm depth was 28.2% higher (p<0.05) than NT. Soil moisture and temperature under CT at 0-5 cm depth were respectively 38.1% and 4.5% higher (p<0.05) than IT. High N rate decreased soil pH at 0-20 cm depth as much as 10%, but increased total soil N at 0-5 cm depth as much as 19% (p<0.05). At 0-10 cm depth, MT with no N had highest exchangeable K, while IT with medium N rate had the lowest (p<0.05). At 0-5 cm depth, MT with no N had highest exchangeable Ca, but it had the lowest (p<0.05) if combined with higher N rate. Microbial biomass C throughout the growing season for NT was consistently highest and it was 14.4% higher (p<0.05) than IT. Compared to IT, Ap horizon of CT after 24 years of cropping was deeper, with larger soil structure and more abundance macro pores. Soybean and corn yields for long-term CT were 64.3% and 31.8% higher (p<0.05) than IT, respectively. Corn yield for long-term N with rate of 100 kg N ha-1 was 36.4% higher (p<0.05) than with no N.Keywords: Conservation tillage, crop yields, N fertilization, soil properties[How to Cite: Utomo M, IS Banuwa, H Buchari, Y Anggraini and Berthiria. 2013.Long-term Tillage and Nitrogen Fertilization Effects on Soil Properties and Crop Yields. J Trop Soils 18 (2): 131-139. Doi: 10.5400/jts.2013.18.2.131][Permalink/DOI: www.dx.doi.org/10.5400/jts.2013.18.2.131] REFERENCESAl-Kaisi and X Yin. 2005. Tillage and crop residue effects on soil carbon dioxide emission in corn- soybean rotation. J Environ Qual 34: 437-445. Pub Med. Barak P, BO Jobe, AR Krueger, LA Peterson and DA Laird. 1997. Effects of long-term soilacidification due to nitrogen inputs in Wisconsin. Plant Soil 197: 61-69.Blake GR and KH Hartge. 1986. Bulk density. In: A Klute (ed). Methods of Soil Analysis. ASA and SSSA. Madison, Wisconsin, USA, pp. 363-375.Blanco-Canqui H and R Lal. 2008. No-till and soil-profile carbon sequestration: an on farm assessment. Soil Sci Soc Am J 72: 693-701. Blanco-Canqui H, LR Stone and PW Stahlman. 2010. Soil response to long-term cropping systems on an Argiustoll in the Central Great Plains. Soil Sci Soc Am J 74: 602-611.Blevins RL, MS Smith, GW Thomas and WW Frye. 1983. Influence of conservation tillage on soil properties. J Soil Water Conserv 38: 301-305.Blevins RL, GW Thomas and PL Cornelius. 1977 Influence of no-tillage and nitrogen fertilization on certain soil properties after 5 years of continuous corn. Agron J 69: 383-386.Blevins, RL and WF Frye, 1993. Conservation tillage: an ecological approach to soil management. Adv Agron 51: 34-77.Brady NC and RR Weil. 2008. The nature and properties of soils. Pearson Prentice Hall. Fourteenth Edition. New Jersey, 965 p.Brito-Vega, H, D Espinosa-Victoria, C Fragoso, D Mendoza, N De la Cruz Landaro and A Aldares-Chavez. 2009. Soil organic particle and presence of earthworm under different tillage systems. J Biol Sci 9: 180-183.Derpch, R 1998. Historical review of no-tilage cultivation of crops. JIRCAS Working Rep. JAPAN Int Res Ctr for Agric Sciences, Ibaraki, Japan 13: 1-18. Diaz-Zorita, M., JH Grove, L Murdock, J Herbeck and E Perfect. 2004. Soil structural disturbance effects on crop yields and soil properties in a no-till production system. Agron J 96: 1651-1659.Dickey EC, PJ Jasa and RD Grisso. 1994. Long-term tillage effect on grain yield and soil properties in a soybean/grain sorghum Rotation. J Prod Agric 7: 465 - 470.Edwards WM, LD, Norton, CE, Redmond. 1988. Characterizing macro pores that affect infiltration into non tilled soil. Soil Sci Soc Am J 52: 483-487.Fernandez RO, PG Fernandez, JVG Cervera and FP Torres. 2007 Soil properties and crop yields after 21 years of direct drilling trials in southern Spain. Soil Till Res 94: 47-54.Fengyun Z, W Pute, Z Xining and C Xuefeng. 2011. The effects of no-tillage practice on soil physical properties. Afr J Biotech 10: 17645-17650. Havlin, JL, JD Beaton, SM Tisdale and WL Nelson. 2005. Soil Fertility and Fertilizer: an Introduction to Nutrient Management. Pearson Prantice Hall. Sevent Edition. Upper Saddle River, New Jersey, 515 p.Karlen DL, NC Wollenhaupt, DC Erbach, EC Berry, JB Swan, NS Eash and JL Jordahl. 1994. Crop residue effects on soil quality following 10-years of no-till corn. Soil Till Res 31: 149-167.Kumar A and DS Yadav. 2005. Effect of zero and minimum tillage in conjunction with nitrogen management in wheat (Triticum aestivum ) after rice (Oryza sativa.). Indian J Agron 50 (1): 54-57.Lal R. 1989. Conservation tillage for sustainable agriculture: tropics versus temper­ate environment. Adv Agron 42: 85-197.Lal R. 1997. Residue management, conservation tillage and soil restoration for mitigating greenhouse effect by CO2 enrichment. Soil Till Res 43: 81-107.Lal R. 2007. Soil science in a changing climate. CSA New 52: 1-9.Mallory J J, RH Mohtar, GC Heathman, DG Schulze and E Braudeau. 2011. Evaluating the effect of tillage on soil structural properties using the pedostructure concept. Geoderma 163: 141-149. doi:10.1016/ j.geoderma. 2011.01.018. 9p.Paustian K, HP Collins and EA Paul. 1997. Management control on soil carbon. In: EA Paul, ET Elliot, K Paustian and CV Cole (eds). Soil Organic Matter in Temperate Agro-ecosystems: Long-term Experiment in North America. CRC Press, pp. 15-50.Rasmussen, KJ. 1999. Impact of ploughless soil tillage on yield and soil quality: A Scandinavian review. Soil Till Res 53: 3-14.Quintero M. 2009. 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Hens, Luc, Nguyen An Thinh, Tran Hong Hanh, et al. "Sea-level rise and resilience in Vietnam and the Asia-Pacific: A synthesis." VIETNAM JOURNAL OF EARTH SCIENCES 40, no. 2 (2018): 127–53. http://dx.doi.org/10.15625/0866-7187/40/2/11107.

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Climate change induced sea-level rise (SLR) is on its increase globally. Regionally the lowlands of China, Vietnam, Bangladesh, and islands of the Malaysian, Indonesian and Philippine archipelagos are among the world’s most threatened regions. Sea-level rise has major impacts on the ecosystems and society. It threatens coastal populations, economic activities, and fragile ecosystems as mangroves, coastal salt-marches and wetlands. This paper provides a summary of the current state of knowledge of sea level-rise and its effects on both human and natural ecosystems. The focus is on coastal urban areas and low lying deltas in South-East Asia and Vietnam, as one of the most threatened areas in the world. About 3 mm per year reflects the growing consensus on the average SLR worldwide. The trend speeds up during recent decades. The figures are subject to local, temporal and methodological variation. In Vietnam the average values of 3.3 mm per year during the 1993-2014 period are above the worldwide average. Although a basic conceptual understanding exists that the increasing global frequency of the strongest tropical cyclones is related with the increasing temperature and SLR, this relationship is insufficiently understood. Moreover the precise, complex environmental, economic, social, and health impacts are currently unclear. SLR, storms and changing precipitation patterns increase flood risks, in particular in urban areas. Part of the current scientific debate is on how urban agglomeration can be made more resilient to flood risks. Where originally mainly technical interventions dominated this discussion, it becomes increasingly clear that proactive special planning, flood defense, flood risk mitigation, flood preparation, and flood recovery are important, but costly instruments. Next to the main focus on SLR and its effects on resilience, the paper reviews main SLR associated impacts: Floods and inundation, salinization, shoreline change, and effects on mangroves and wetlands. The hazards of SLR related floods increase fastest in urban areas. This is related with both the increasing surface major cities are expected to occupy during the decades to come and the increasing coastal population. In particular Asia and its megacities in the southern part of the continent are increasingly at risk. The discussion points to complexity, inter-disciplinarity, and the related uncertainty, as core characteristics. An integrated combination of mitigation, adaptation and resilience measures is currently considered as the most indicated way to resist SLR today and in the near future.References Aerts J.C.J.H., Hassan A., Savenije H.H.G., Khan M.F., 2000. Using GIS tools and rapid assessment techniques for determining salt intrusion: Stream a river basin management instrument. 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Petryanin, Aleksey V. "Review of the official opponent to a PhD (Law) thesis (major 12.00.08): Buchaev S. M. “Criminological issues of counteracting the process of forming a personality of a terrorist”." Actual Problems of Economics and Law 13, no. 3 (2019). http://dx.doi.org/10.21202/1993-047x.13.2019.3.1473-1483.

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Conference papers on the topic "Thesis Aero 1993 M.S"

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Falchetti, F., H. Quiniou, and L. Verdier. "Aerodynamic Design and 3D Navier-Stokes Analysis of a High Specific Flow Fan." In ASME 1994 International Gas Turbine and Aeroengine Congress and Exposition. American Society of Mechanical Engineers, 1994. http://dx.doi.org/10.1115/94-gt-477.

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Abstract:
Advanced research is currently being conducted at Snecma to design a swept wide chord fan blade with a very high specific flow value of 230 kg/s/m2 at the aero design point instead of 212 kg/s/m2 on current turbofan engines. This concept has the potential benefit of higher thrust than conventional engines for a given value of the fan diameter. This induces potential advantages in terms of performance (reduced nacelle drag) and installation under the wings. These advantages are subject to the condition that we retain high fan bypass efficiency with axial Mach number close to 0.8. The intensive use of 3D Euler and 3D Navier-Stokes blade to blade computations in the aero design makes it possible to overcome this difficulty. This paper describes the aero optimization of a swept fan blade with a specific flow of 230 kg/s/m2, a corrected tip speed of 350 m/s and a bypass pressure ratio of 1.45. Applications of the most recent numerical methods are presented, including 3D Navier-Stokes blade to blade computations.
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