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Kumar, Sandeep
- Nanocrystalline Silica from Termite Mounds
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PDF Views:92
Authors
Affiliations
1 Institute of Nano Science and Technology, Habitat Centre, Phase-X, Sector–64, Mohali 160 062, IN
2 Department of Chemistry, Indian Institute of Technology, Delhi, Hauz Khas, New Delhi 110 016, IN
3 Department of Chemistry, Hindu College, University of Delhi, Delhi 110 007, IN
1 Institute of Nano Science and Technology, Habitat Centre, Phase-X, Sector–64, Mohali 160 062, IN
2 Department of Chemistry, Indian Institute of Technology, Delhi, Hauz Khas, New Delhi 110 016, IN
3 Department of Chemistry, Hindu College, University of Delhi, Delhi 110 007, IN
Source
Current Science, Vol 106, No 1 (2014), Pagination: 83-88Abstract
To develop a better understanding of the physical properties and microstructures of the termite hill soils, we have carried out studies on the soil samples collected from two locations: near Dehradun, Utta-rakhand and near Hauz Khas, New Delhi. Their ele-mental composition and microstructure were studied using different instrumentation techniques, such as powder X-ray diffraction, field emission scanning electron.Microscopy, transmission electron microscope (TEM) and energy-dispersive analysis of X-ray (EDAX). α-Quartz (SiO2) was present in both the samples, while the sample collected from Hauz Khas, Delhi also con-tained β-cristobalite phase of SiO2. TEM-EDAX showed that termite hill soil consisted of silica (quartz), aluminium oxide, manganese oxide and iron oxide along with small percentage of potassium and calcium. Our studies highlight the potential to gene-rate α-quartz from all termite hills. It is also possible to obtain the less common β-cristobalite form of silica in certain termite mounds.
Keywords
β-Cristobalite, α-Quartz, Termite Mound, Silica.- Spatial Distribution pf Landslides Vis-à-Vis Epicentral Distribution of Earthquakes in The Vicinity of The Main Central Thrust Zone, Uttarakhand Himalaya, India
Abstract Views :156 |
PDF Views:81
Authors
Affiliations
1 Wadia Institute of Himalayan Geology, Dehradun 248 001, IN
1 Wadia Institute of Himalayan Geology, Dehradun 248 001, IN
Source
Current Science, Vol 120, No 12 (2021), Pagination: 1927-1932Abstract
Landslides and related mass movement activities along with earthquakes are common in the Himalayan terrain. The distribution of seismic activities in the vicinity of the Main Central Thrust (MCT) is well known. However, in order to assess the relationship between these seismic events and landslides, the spatial distribution of landslides and earthquake events (magnitude >1.5) on either side of the MCT zone was evaluated. It has been observed that seismic events of magnitude <2.1 are clustered around the 1991 Uttarkashi earthquake rupture, 1999 Chamoli earthquake rupture and around Munsiyari. The zone surrounding 1999 Chamoli earthquake rupture indicates the highest earthquake and landslide density of ∼75% and 53% respectively.Keywords
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