The Roles of Agglomeration Economies and Comparative Advantage in the Regional Distribution of FDI in China.

Master'sMASTER OF SOCIAL SCIENCE

An Online Distributed Boundary Detection and Classification Algorithm for Mobile Sensor Networks

We present a novel online distributed boundary detection and classification algorithm in order to improve accuracy of boundary detection and classification for mobile sensor networks. This algorithm is developed by incorporating a boundary detection algorithm and our newly proposed boundary error correction algorithm. It is a fully distributed algorithm based on the geometric approach allowing to remove boundary errors without recursive process and global synchronization. Moreover, the algorithm allows mobile nodes to identify their states corresponding to their positions in network topologies, leading to self-classification of interior and exterior boundaries of network topologies. We have demonstrated effectiveness ofthis algorithm in both simulation and real-world experiments and proved that the accuracy of the ratio of correctly identified nodes over the total number of nodes is 100%

Low-power pedestrian detection system on FPGA

Pedestrian detection is one of the key problems in the emerging self-driving car industry. In addition, the Histogram of Gradients (HOG) algorithm proved to provide good accuracy for pedestrian detection. Many research works focused on accelerating HOG algorithm on FPGA(Field-Programmable Gate Array) due to its low-power and high-throughput characteristics. In this paper, we present an energy-efficient HOG-based implementation for pedestrian detection system on a low-cost FPGA system-on-chip platform. The hardware accelerator implements the HOG computation and the Support Vector Machine classifier, the rest of the algorithm is mapped to software in the embedded processor. The hardware runs at 50 Mhz (lower frequency than previous works), thus achieving the best pixels processed per clock and the lower power design

Investment on environmental social and governance activities and its impact on achieving sustainable development goals: evidence from Chinese manufacturing firms

Achieving sustainable development goals (SDGs) is a global requirement that attracts new researchers and regulators. So, the current research investigates the impact of investment on the environment, social, and governance (ESG) activities on the achievement of SDGs of the Chinese manufacturing companies. The current article also examines the mediating impact of organizational effectiveness among the nexus of investment in ESG activities and the achievement of SDGs of the Chinese manufacturing companies. The current research has taken the questionnaires to gather the data and used the smart-PLS to analyze the data. The results exposed that investment in the environment and social activities have a positive impact on the achievement of SDGs. The findings also revealed that the organizational effectiveness significantly mediates among the nexus of investment in the environment and social activities and the achievement of SDGs of the Chinese manufacturing companies. This study provides help to the relevant authorities to achieve the SDGs using the investment in ESG activities

ASSESSMENT OF GEOMORPHIC PROCESSES AND ACTIVE TECTONICS IN CON VOI MOUNTAIN RANGE AREA (NORTHERN VIETNAM) USING THE HYPSOMETRIC CURVE ANALYSIS METHOD

the Day Nui Con Voi (DNCV) area of Vietnam. For this purpose, a spatial database was collected and constructed, including DEM (Digital Elevation Model) and a geological map. The hypsometric curve (HC) analysis method and its statistical moments were adopted to use for the assessment. These methods have been widely used for the assessment of geomorphic processes and active tectonics in many areas in the world showing promising results. A total of 44 sub-basins of the Red River and the Chay river were analyzed. The result shows that 3 curve-types such as "straight- shape", "S- shape", and concave were found; with the concave curve being the dominant and widely distributed in the northeast side and in the south of the southwestern side of the study area. The hypsometric integral (HI) values are rather small with the largest value is 0.37 and the smallest one is 0.128. Other statistical moments of the hypsometric curve, i.e. skew (SK), kurtosis (KUR), and the density function (density skew - DSK and density kurtosis-DKUR) show great values, which increased in the south direction of the area study. Accordingly, recent active tectonics (uplift-lower) in the study area is generally weak; however, they are also not completely homogeneous and can be distinguished by different levels. The southwestern side is being lifted higher than the northeastern side. The northern part is being lifted larger than the southern part. In the region, the uplift activities were increased gradually in the Pliocene-Quaternary and could have stopped at certain time in the past. The current geomorphic processes are mainly headward erosion in the upstream.References Allen, C.R., Gillepie, A.R., Han, Y., Sieh, K.E., Zhu, C., 1984. Red River and associated faults, Yunnan province, China: Quaternary geology, slip rates, and seismic hazard, Geological Society of America Bulletin,  686-700, 21 fig.Azor, A., Keller, E.A., Yeats, R.S., 2002. Geomorphic indicators of active fold growth: South Mountain-Oak Ridge anticline, Ventura basin, southern California. Geological Society of America Bulletin 114, 745-753.Chen, Y.C., Sung, Q., Cheng, K.Y., 2003. Along-strike variations of morphotectonic features in the Western Foothills of Taiwan: tectonic implications based on stream gradient and hypsometric analysis. Geomorphology 56, 109-137.Delcaillau, B., Deffontaines, B., Floissac, L., Angelier, J., Deramond, J., Souquet, P., Chu, H.T., Lee, J.F., 1998. Morphotectonic evidence from lateral propagation of an active frontal fold; Pakuashan anticline, foothills of Taiwan. Geomorphology 24, 263-290.Delcaillau, B., Laville, E., Amhrar, M., Namous, M., Dugué, O., Pedoja, K., 2010. Quaternary evolution of the Marrakech High Atlas and morphotectonic evidence of activity along the Tizi N'Test Fault, Morocco. Geomorphology 118, 262-279.El Hamdouni, R., Irigaray, C., Fernández, T., Chacón, J., Keller, E.A., 2008. Assessment of relative active tectonics, southwest border of the Sierra Nevada (southern Spain). Geomorphology 96, 150-173.Font, M., Amorese, D., Lagarde, J.L., 2010. DEM and GIS analysis of the stream gradient index to evaluate effects of tectonics: the Normandy intraplate area (NW France). Geomorphology 119, 172-180.Gardner, T.W., Sasowsky, K.C., Day, R.L., 1990. Automated extraction of geomorphometric properties from digital elevation models. Zeischrift für Geomorphologie Supplemental Band 80, 57-68.Harlin, J.M., 1978. Statistical moments of the hypsometric curve and its density function. Mathematical Geology 10, 59-72.Howard, A.D., 1990. Role of hypsometry and planform in basin hydrologic response. Hydrological Processes 4, 373-385.Huang, X.J., Niemann, J.D., 2006. Modelling the potential impacts of groundwater hydrology on long-term drainage basin evolution. Earth Surface Processes and Landforms 31, 1802-1823.Joshi, P.N,. Maurya, D.M., Chamyal, L.S., 2013. Morphotectonic segmentation and spatial variability of neotectonic activity along the Narmada-Son Fault, Western India: Remote sensing and GIS analysis. Geomorphology 180-181 (2013) 292-306.Keller, E.A., Pinter, N., 2002. Active Tectonics. Earthquakes, Uplift and Landscape. Prentice Hall, New Jersey, 362.Le Duc An, 2003. About the exhumation of metamorphic rocks of Con Voi range. Journal of Sciences of the Earth,No.1, 93-95 (In Vietnamese with English abstract).Le Duc An, Dao Dinh Bac, Uong Dinh Khanh, Vo Thinh, Tran Hang Nga, Ngo Tuan Anh, Nguyen Thi Le Ha, 2004. Geomorphology of Red River Fault Zone and natural hazard.P 459-532. Science and Technics Publishing House, Hanoi (In Vietnamese with English abstract).Le Duc An, Lai, Huy Anh, Vo Thinh, Ngo Tuan Anh, Do Minh Tuan, Tran Hang Nga, 2001. Steps of relief of Convoi Mountain characteristics. Journal of Sciences of the Earth, 23(2), 97-104. (In Vietnamese with English abstract).Leloup, P.H., Arnaud, N., Lacassin, R., Kienast, J.R., Harrison, T.M., Trinh, P.T., Replumaz, A., Tapponnier, P., 2001. New constraints on the structure, thermochronology, and timing of the Ailao Shan-Red River shear zone, SE Asia, Journal of Geophysical Research, B, v. 106, 6683-6732.Leloup, P.H., Chen Wenji, Harrison, T.M., Tapponnier, P., 1994. Timing of shear sense inversion along the Red River fault zone. Int. Workshop on Seismotectonics and Seismic Hazard in South East Asia, Hanoi.Leloup, P.H., Lacasin, Tapponnier, P., Scharer, U., Dalai, Z., Xaohan, L., Zhangshan, Shaocheng, J., Trinh, P.T., 1995. The Ailao Shan -  Red Rive shear zone (Yunnan, China), Tertiary transform boundary of  Indochina. Tectonophysics, v. 251,  pp. 3-84.Leloup, P.H., Lacassin, R., Tapponnier, P., Harrison, T.M., 2001. Comment on “Onset timing of left-lateral movement along the Ailao Shan±Red River Shear Zone: 40Ar/39Ar dating constraint from the Nam Dinh Area, northeastern Vietnam” by Wang et al., 2000. Journal of Asian Earth Sciences 18, 281-292. Journal of Asian Earth Sciences 20, 95-99.Lifton, N. A., Chase, C.G., 1992. Tectonic, climatic and lithologic influences on landscape fractal dimension and hypsometry: implications for landscape evolution in the San Gabriel Mountains, California. Geomorphology 5, 77-114.Luo, W., 1998. Hypsometric analysis with a geographic information system. Computers Geosciences, Vol. 245, No. 8, 815-821.Luo, W., 2000. Quantifying groundwater- sapping landforms with a hypsometric technique. Journal of Geophysical Research, Vol. 105, No. El, Pages 1685-1694, January 25.Mahmood, S. A., and Gloaguen, R.,  2012. Appraisal of active tectonics in Hindu Kush: Insights from DEM derived geomorphic indices and drainage analysis. Geoscience Frontiers 3(4), 407-428.Moglen, G.E., Bras, R.L., 1995. The effect of spatial heterogeneities on geomorphic expression in a model of basin evolution. Water Resources Research 31, 2613-2623.Ngo Van Liem, 2011. Characteristics of landform evolution in relation to recent geodynamics along the Red River Fault Zone, Doctorate thesis, Institute of Geological Sciences, Hanoi (In Vietnamese with English abstract).Ngo Van Liem, Phan Trong Trinh, Hoang Quang Vinh, 2006. The active faults and the maximum earthquakes of the Red River Fault zone in Lao Cai-Yen Bai area, Journal of Sciences of the Earth, Vol. 28, (2), 110-120 (In Vietnamese with English abstract).Ngo Van Liem, Phan Trong Trinh, Nguyen Van Huong, Nguyen Cong Quan, Tran Van Phong, Nguyen Phuc Dat, 2016. Analyze the correlation between the geomorphic indices and recent tectonic active of the Lo River fault zone in southwest of Tam Dao range. Vietnam Journal of Earth Sciences. Vol. 38, No. 1, 1-13 (In Vietnamese with English abstract).Nguyen Quoc Cuong., Zuchiewicz, W., Tokarski. A. K., 1999. Morphotectonic evidence for right-lateral normal slip in the Red River Fault Zone: insights from the study on Tam Dao fault scarp (Viet Nam), J. Geology, Seri B, 13-14, 57-59.Nguyen Xuan Nam, 2015. Quaternary Geology characteristics, present-day tectonic geomorphology of the Da river valley from HoaBinh to Viet Tri and correlation with geological hazards. Doctorate Thesis. Hanoi University of Mining and Geology (In Vietnamese with English abstract).Ohmori, H., 1993. Changes in the hypsometric curve through mountain building resulting from concurrent tectonics and denudation. Geomorphology 8, 263-277.Pedrera, A., Pérez-Peña, J.V., Galindo-Zaldívar, J., Azañón, J.M., Azor, A., 2009. Testing the sensitivity of geomorphic indices in areas of low-rate active folding (eastern Betic Cordillera, Spain). Geomorphology 105, 218-231.Pérez-Peña, J.V., Azañón, J.M., Azor, A., 2009. CalHypso: An ArcGIS extension to calculate hypsometric curves and their statistical moments. Applications to drainage basin analysis in SE Spain. Computers Geosciences 35, 1214-1223.Phan Trong Trinh, Hoang Quang Vinh, Leloup Philippe Hervé, Giuliani, G., Vincent Garnier., Tapponnier, P., 2004. Cenozoic deformation, thermodynamic evolution, slip mechanism of Red River shear zone and ruby formation. Science and Technics Publishing House, Hanoi. P5-72 (In Vietnamese with English abstract).Phan Trong Trinh, Ngo Van Liem, Nguyen Van Huong, Hoang Quang Vinh, Bui Van Thom, Bui Thi Thao, Mai Thanh Tan, Nguyen Hoang, 2012. Late Quaternary tectonics and seismotectonics along the Red River fault zone, North Vietnam. Earth-Science Reviews 114, 224-235.Phan Van Quynh, Vo Nang Lac, and Tran Ngoc Nam, 1995. Some features of late Paleozoic-Cenozoic deformation tectonics on the territory of Vietnam and neighboring areas. In: Geology, Mineral Resources and Petroleum of Vietnam. Geological Survey of Vietnam, Hanoi, 171-183 (in Vietnamese with an English abstract).Phung Thi Thu Hang, 2011. Study and comparison recent active tectonics between the Red River and the Dien Bien - Lai Chau Fault Zones base on geomorphic indices. Master thesis. VNU University of Science, Hanoi.Shahzad, F., and Gloaguen, R., 2011. TecDEM: AMATLAB based tool box for tectonic geomorphology, Part 1: Drainage network preprocessing and stream profile analysis. Computers Geosciences 37, 250-260.Strahler, A.N., 1952. Hypsometric (area-altitude) analysis of erosional topography. Geological Society of America Bulletin 63, 1117-1142.Strahler, A.N., 1957. Quantitative analysis of watershed geomorphology. Transactions of the American Geophysical Union 38, 913-920.Tran Dinh To, 2002. The characterize of  Neotectonics of Red River-Chay River Fault Zone. Doctorate Thesis, Institute of Geological Sciences, Hanoi, (In Vietnamese with English abstract).Tran Dinh To, Duong Chi Cong, Vy Quoc Hai, Matthias Becker, Marina Neuman, 2003. Activity  of Red River fault zone at Tam Dao-Ba Vi derived from GPS data (1994-1996-1998-2000). Journal of Sciences of the Earth, 25(4)PC, 511-515 (In Vietnamese with English abstract).Tran Dinh To, Nguyen Trong Yem, 2001.Amplitude and rate of slip of the Red River Zone in late Cenozoic. Journal of Sciences of the Earth, 23(4), 334-353. (In Vietnamese with English abstract).Tran Ngoc Nam, 1999. Red River Fault zone - focus of the scientific debate. Part II: P-T-t paths and post-metamorphic exhumation, Journal of Sciences of the Earth, No.3, 161-167 (In Vietnamese with English abstract).Tran Ngoc Nam, 2002. Exhumation mechanisms of the Day Nui Con Voi. Journal of Sciences of the Earth, No.3,  286-288 (In Vietnamese with English abstract).Tran Ngoc Nam, Mitsuhiro Toriumi, TetsumaruItaya, 1998. P-T-t paths and post-metamorphic exhumation of the Day Nui Con Voi shear zone in Vietnam. Tectonophysics 290, 299-318.Tran Ngoc Nam., Toriumi, M., Sano, Y., Terada, K., Ta, T.T.,, 2003. 2.9, 2.36, and 1.96 Ga zircons in orthogneiss south of the Red River shear zone in Viet Nam: evidence from SHRIMP U-Pb dating and tectonothermal implications. Journal of Asian Earth Sciences 21, 743-753.Trinh Thi Thuy, 2014. Assessment of modern tectonic activity of the Son La fault zones on the basis of tectonic geomorphology. Master thesis. The University of Science - Vietnam National University, Hanoi (In Vietnamese with English abstract).Wang, P.L., Lo, C.H., Chung, S.L., Lee T.Y., Lan, C.Y., Thang, T.V., 2000. Onset timing of left-lateral movement along the Ailao Shan±Red River Shear Zone: 40Ar/39Ar dating constraint from the Nam Dinh Area, northeastern Vietnam. Journal of Asian Earth Sciences. Volume 18, Issue 3, 1 June 2000, 281-292.Willgoose, G., 1994. A physical explanation for an observed area-slope-elevation relationship for catchments with declining relief. Water Resources Research 30, 151-159.Willgoose, G., Hancock, G., 1998. Revisiting the hypsometric curve as an indicator of form and process in transport-limited catchment. Earth Surface Processes and Landforms 23, 611-623.Zuchiewicz, W., Nguyen Quoc Cuong, Jerzy Zasadni, Nguyen Trong Yem, 2013. Late Cenozoic tectonics of the Red River Fault Zone, Vietnam, in the light of geomorphic studies. Journal of Geodynamics 69, 11-30. 

Effects of protein levels of commercial diets on the growth performance and survival rate of rabbitfish (Siganus guttatus) at the nursing stage

This study aimed to determine the effect of a commercial diet's protein level on the fry-to-fingerling stage. Thirty days-old fries having the initial length and weight of 18.25 ± 0.15 mm fish-1 and 0.036 ± 0.50 g fish-1 respectively have been used in this study. Diet having three protein levels i.e. 30% (trial 1 as control), 35% (trial 2), 40% (trial 3), and 45% (trial 4), respectively, have been used to evaluate the effect of protein, and each trial has been repeated three times. During the study, stocking density was allocated to 1000 fish per composite tank with a volume of 1 m3. After 30 days of rearing, the weight of fingerlings in trial 1 reached up to 1.50 ± 0.02 g fish-1 and it was recorded as 1.52 ± 0.01g for trial 2, these two were lower than that of trials 3 and 4, where fingerling weight was reported 1.69 ± 0.01 and 1.58g fish-1 respectively and obtained the best weight compared to others. The length of fingerlings at the end of the experimental period was also changed in different trials and it was recorded 47.12; 46.92; 50.97; and 48.89 mm fish-1 for trail 1, 2, 3, and 4 respectively, among the tested combinations lower fingerlings length was recorded for trial 2 (35% CP), but it is not significantly different for trial 1 and 2 and a significant difference (P < 0.05) was reported for trail 2, 3, and 4. The survival rate of fingerlings ranged from 67.27 to 72.33%. Meanwhile, the herd distribution coefficient variation (CVW) in the treatment using 40% protein (trial 3) was the highest at 72.33% (p < 0.05). The results of the study can be concluded that the level of protein has a significant effect on the various growth parameters of fingerlings

Synthesis of Gold Nanobipyramids by Seed-mediated Method and Santibacterial Activities

Metallic nanoparticles as antibacterial agents have been studied for several years. The most used antibacterial nanoparticles are silver nanoparticles. The mechanisms and  antibacterial properties of silver nanoparticles are well known, but the effects of gold nanoparticles, especially gold Nano bipyramids, are not considered. In this research, we synthesized gold nanobipyramids (NBPs) by seed mediated method using surfactant cetyltrimethylammonium bromide (CTAB). After preparing, gold nanobipyramids is removed CTAB and modified the surface using polyethylene glycol, polyvinyl alcohol and chitosan as the stabilizers. Besides, antibacterial effects of gold nanobipyramids on both Escherichia coli (Gram negative) and Staphylococcus aureus (Gram positive) are investigated in this paper. The results show that gold nanobipyramids have good antibacterial activities even at low concentration. The optimal concentration of stabilizers and gold nanobipyramids in antibacterial activities are also studied in this paper

GRADIENT KIẾN TẠO HIỆN ĐẠI KHU VỰC NINH THUẬN VÀ LÂN CẬN

The estimation of the present day tectonic movement and tectonic gradient (strain rate) has an important practical signification in the assessment of active fault and seismic hazards for the selection of Ninh Thuan nuclear power plant. Based on the three campaigns of GPS measurement between 2012 - 2013, we used BERNESE 5.0 software to determine present day slip rates of 13 stations in ITRF08 frame. The GPS stations move eastwards at the slip rates of 22 - 25 mm/yr, southwards at the velocities of 5 - 10 mm/yr. The standard errors in latitudinal and longitudinal directions are 1.2 mm/yr and 0.9 mm/yr, respectively. Combined with GPS data from the project of the study on actual geodynamics in Tay Nguyen TN3/06, we determined the strain rate ranging from 50 to 100 nanostrains with the standard error of 50 nanostrains. The direction of  maximum compressive strain rate is from northwest - southeast to east - west.Đánh giá vận tốc chuyển động kiến tạo hiện đại và gradient kiến tạo hiện đại có ý nghĩa thực tiễn quan trọng trong việc đánh giá đứt gãy hoạt động nguy hiểm động đất phục vụ xây dụng nhà máy điện hạt nhân Ninh Thuận. Trên cơ sở đo 3 chu kỳ GPS vào các năm 2012 - 2013, sử dụng phần mềm BERNESE 5.0, chúng tôi đã xác lập được vận tốc chuyển động kiến tạo hiện đại tại 13 điểm đo GPS trong khu vực lân cận bao gồm kéo dài từ Nha Trang tới đảo Phú Quý. Vận tốc chuyển dịch kiến tạo hiện đại về phía đông thay đổi từ 22 - 25 mm/năm và chuyển dịch về phía nam với vận tốc giao động từ 5 - 10 mm/năm trên hệ tọa độ toàn cầu ITRF08. Sai số vận tốc chuyển dịch kiến tạo về phía đông giao động trong khoảng 1,2 - 1,5 mm/năm và về phía nam giao động trong khoảng 0,9 - 1,2 mm/năm. Liên kết với giá trị đo GPS từ đề tài nghiên cứu địa động lực hiện đại khu vực Tây Nguyên mã số TN3/T06, chúng tôi đã xác định được giá trị vận tốc biến dạng giao động từ 50 nano tới 100 nano biến dạng với sai số giao động trong khoảng 50 nano biến dạng. Trục biến dạng nén cực đại giao động theo phương thay đổi từ bắc nam sang đông bắc - tây nam. Trục biến dạng căng cực đại có phương thay đổi từ tây bắc - đông nam sang phương đông - tây