Skip to main content

IIT Delhi-University of Queensland International Joint PhD with Scholarships and fellowship



IIT Delhi-University of Queensland International Joint PhD in Science, Engineering, Management, Humanities: Apply by March 22
Start your future on Coursera today.
     
BY: USHA | 24 Feb 2020 11:17 AM

 
The University of Queensland, Australia and IIT Delhi have created a joint research programme titled UQ-IITD Academy of Research (UQIDAR).

UQIDAR will attract the best global talent, including elite students, academics, researchers and scientists to work on goal-directed, cross-disciplinary grand challenges that are of interest to Australia, India and the global community and that also align with The University of Queensland (UQ) and Indian Institute of Technology (IITD) research strengths. UQIDAR will enable UQ and IITD to enrol the brightest and most talented students in a joint PhD with joint supervision from both institutions. It is anticipated that the majority of students (i-students) will be recruited into the joint-PhD program in Delhi, and there will be a small cohort of Australia-anchored scholars (q-students).

i-students will spend 3 years in India and a minimum of one year in Australia while
q-students will spend 3 years in Australia and one year in India.
It is expected that candidature will be a maximum of 4 years in all disciplines, depending on a students progress, with scholarships offered for a maximum of 4 years. Both i-students and q-students will be expected to undertake some coursework. Upon successful completion of the program, students will be offered a PhD degree from both UQ and IITD.

Students of the Academy will
Gain a joint global qualification from two institutions (UQ and IITD) in 4 years;
Receive a generous scholarship;
Be in a position to take advantage of world-class facilities and resources and gain exposure to a new research ecosystem, network and environment; and
Benefit from global expertise via dual supervision between UQ and IITD as well as possible industry input.
The collaboration will involve strong industry linkages whereby industry will be involved in supporting PhD students. Industry supported PhD scholars will work on challenging research problems posed and defined by industry partners of the UQIDAR. Industry supervisors will co-guide the students along with UQ and IITD supervisors. The collaboration will also enable the establishment of a mobility or fellowship scheme to enable academics and postdoctoral fellows to spend time at each institute, expanding research linkages and offering career development opportunities for early career researchers.

Comments

Popular posts from this blog

Geography of Landslides. Mitigation and Resilience.

A landslide is a geological event in which a mass of rock, earth, or debris moves down a slope under the force of gravity. Landslides can range in size from small to large and can be triggered by natural events such as heavy rainfall, earthquakes, or volcanic activity, or by human activities such as construction or mining. The geography of landslides is affected by a variety of factors that can increase the likelihood of landslides occurring in a particular area. These factors include slope angle and steepness, the type of soil and rock present, the climate and weather patterns of the region, the presence or absence of vegetation, and human activities such as construction, mining, and deforestation. Areas with steep slopes are more prone to landslides because gravity has a stronger effect on loose soil and rock, making it more likely to move downhill. Similarly, areas with loose, sandy soil or weak, fractured rock are more prone to landslides because they are less stable and more easil...

Geography of Flood. Types. Charector.

The geography of floods refers to the characteristics and patterns of floods in different geographic regions. Floods can occur in various landscapes, such as mountains, plains, coastal areas, and urban environments. The geography of a region plays a significant role in determining the frequency, magnitude, and impacts of floods. Some of the factors that influence the geography of floods include: Topography: The shape and elevation of the land can affect the flow and accumulation of water during a flood. For example, flat terrain can lead to slow-moving and widespread flooding, while steep slopes can result in flash floods and landslides. Climate: Regions with high rainfall or snowmelt can experience more frequent and intense floods, while dry regions may experience flash floods due to sudden, heavy rainfall. Hydrology: The characteristics of a river basin, such as its size, shape, and water flow, can influence the severity of a flood. For example, large river basins with extensive floo...

Landslides. USGS

Landslides. TYPES OF LANDSLIDES The term "landslide" describes a wide variety of processes that result in the downward and outward movement of slope-forming materials including rock, soil, artificial fill, or a combination of these. The materials may move by falling, toppling, sliding, spreading, or flowing. The animated GIF shows a graphic illustration of different types of landslides, with the commonly accepted terminology describing their features. The various types of landslides can be differentiated by the kinds of material involved and the mode of movement.

Flood prone regions India

Floods are natural disasters characterized by the overflow of water onto normally dry land. Various factors contribute to floods, including intense rainfall, rapid snowmelt, storm surges from coastal storms, and the failure of dams or levees. The geographical explanation involves understanding the key components of flood-prone regions: 1. Proximity to Water Bodies:    Flood-prone regions are often situated near rivers, lakes, or coastal areas. These locations are more susceptible to flooding as they are in close proximity to large water sources that can overflow during heavy precipitation or storms. 2. Topography:    Low-lying areas with gentle slopes are prone to flooding. Water naturally flows to lower elevations, and flat terrains allow water to accumulate easily. Valleys and floodplains are common flood-prone areas due to their topographical characteristics. 3. Rainfall Patterns:    Regions with high and concentrated rainfall are more likely to experience flooding. Intense and prol...

Volcano

Large magma chamber Bedrock Conduit (pipe) Base Sill Dike Layers of ash emitted by the volcano Flank Layers of lava emitted by the volcano Throat Parasitic cone Lava flow Vent Crater Ash cloud