Implications of new $$^{40}\hbox {Ar}/^{39}\hbox {Ar}$$ age of Mallapur Intrusives on the chronology and evolution of the Kaladgi Basin,Dharwar Craton,India

The Kaladgi Basin on the northern edge of the Dharwar craton has characters diverse from the other epicratonic Purana basins of Peninsular India. Sedimentological studies in the basin have established the presence of three cycles of flooding separated by an event of intra-basinal deformation accompanied by low grade incipient metamorphism. The overall structural configuration of the basin indicates its development by supracrustal extension accompanied by shearing in a trans-tensional regime during the Mesoproterozoic. This was followed by sagging that yielded Neoproterozoic sedimentation in a successor nested basin. \(^{40}\)Ar/\(^{39}\)Ar dating of an intrusive mafic dyke along the axial plane of a fold has yielded a plateau age of \(1154{\pm }4\,\hbox {Ma}\). This helps constraint the age of the various events during the evolution of this basin.     

A coupled 3‐dimensional bonded discrete element and lattice Boltzmann method for fluid‐solid coupling in cohesive geomaterials

This paper presents a 3D bonded discrete element and lattice Boltzmann method for resolving the fluid‐solid interaction involving complicated fluid‐particle coupling in geomaterials. In the coupled technique, the solid material is treated as an assembly of bonded and/or granular particles. A bond model accounting for strain softening in normal contact is incorporated into the discrete element method to simulate the mechanical behaviour of geomaterials, whilst the fluid flow is solved by the lattice Boltzmann method based on kinetic theory and statistical mechanics. To provide a bridge between theory and application, a 3D algorithm of immersed moving boundary scheme was proposed for resolving fluid‐particle interaction. To demonstrate the applicability and accuracy of this coupled method, a benchmark called quicksand, in which particles become fluidised under the driving of upward fluid flow, is first carried out. The critical hydraulic gradient obtained from the numerical results matches the theoretical value. Then, numerical investigation of the performance of granular filters generated according to the well‐acknowledged design criteria is given. It is found that the proposed 3D technique is promising, and the instantaneous migration of the protected soils can be readily observed. Numerical results prove that the filters which comply with the design criteria can effectively alleviate or eliminate the appearance of particle erosion in dams.     

Strontium isotopic composition of the Madera Formation (Pennsylvanian) near Albuquerque,New Mexico

⁸⁷Sr/⁸⁶Sr ratios of fourteen unaltered limestone and six fossil samples show a range of 0.7066-0.7118 for the depositional water of the Middle to Upper Pennsylvanian Madera Formation. The variation of these ⁸⁷Sr/⁸⁶Sr ratios may be due to the restricted depositional basin and nature of the source of the Madera Formation.While fossil and limestone samples are equally good for determination of strontium isotopic composition of depositional waters, leaches of calcareous shales contain significant amount of ⁸⁷Sr leached from the noncarbonate fraction during acid treatment.     

Vibration rotation bands of SiO in sunspots

The equivalent widths of P(51) and R(43) lines of the 1-0 and P(45) and R(56) lines of the 2-1 vibration rotation bands of SiO near 8 m region, have been computed for Zwaan's (1974) sunspot model at the centre of the disc. The predicted equivalent widths suggest a possible presence of these SiO bands in the sunspot spectrum.     

Unsteady hydromagnetic thermal boundary layer flow

Unsteady hydromagnetic thermal boundary layer flow past a non-conducting infinite porous wall in presence of a transverse magnetic field is considered. The magnetic Reynolds number of the flow is taken to be small enough so that the induced magnetic field is negligible. It is assumed that the normal velocity of suction/injection at the wall varies att ^?/12. Solution of the problem, in the form of power series, is obtained for two cases:

1. When the wall temperature is the same as that of the free-stream, and
2. When the difference in the temperatures of the wall and that of the free-stream varies as some power of time. The variations of the skin-friction, the temperature and the rate of heat transfer are shown graphically followed by a quantitative discussion.

     

Bangladeshi American Response to the 1998 Status of Forces Agreement (SOFA): An Assessment*

Following the devastating flood in 1998, the U.S. government proposed a Status of Forces Agreement (SOFA) to the Bangladesh government. Accepting the 1998 SOFA would have allowed entry of U.S. troops in Bangladesh without passports or visas and without requiring declaration of military hardware. This would have facilitated American forces support for relief operations and rehabilitation of disaster victims in the shortest possible time. Unfortunately, the Bangladesh government rejected the U.S. terms outlined in the 1998 proposal. A sample survey was conducted among Bangladeshi Americans to examine their opinions regarding the 1998 SOFA. Survey data reveals that slightly over 58 percent of the respondents supported signing the SOFA. Reasons for their support or opposition to the U.S. proposal are also presented. Statistical analyses suggest that whether respondents have studied or are currently studying in the United States emerged as the most significant factor associated with approval or disapproval of the 1998 SOFA. Implications of the study findings are also discussed.     

Post-Cyclone Sidr illness patterns in coastal Bangladesh: an empirical study

After the landfall of Cyclone Sidr along the southwestern coast of Bangladesh on November 15, 2007, emergency and public health personnel within and beyond Bangladesh anticipated a massive outbreak of water-borne and other diseases in most affected areas. Fortunately, such an outbreak did not occur. The objectives of this paper are to examine the extent and pattern of illnesses experienced by Cyclone Sidr survivors in the aftermath of its landfall and to investigate household and individual-level factors associated with such illnesses. Based on face-to-face interviews conducted among 277 randomly selected Sidr survivors living in the four most severely impacted coastal districts, this study found that the post-cyclone incidence of water-borne, respiratory, and other diseases was not unusually high. Only 52 persons suffered Sidr-related illnesses, and their illnesses were significantly associated with household income, and gender and age of the Sidr survivors. A major outbreak of such diseases was largely avoided because of the proper distribution of food and safe drinking water, as well as the timely implementation of health care intervention measures. This important finding will aid relevant authorities in successfully responding to outbreaks of diseases following a future extreme event in Bangladesh and perhaps elsewhere.     

Time-dependent multilaminate model of rocks—a numerical study of deformation and failure of rock masses

A new model for rocks and rock-like material with multiple planes of weakness is proposed. The behaviour of the assembly applies tensile and Mohr-Coulomb shear limits on each such plane with possible strain dependence of frictional properties. The visco-plastic algorithm which allows the incorporation of time effects is used to obtain static solutions. The model is illustrated in actual context by applications to stability of rock slopes and behaviour of tunnels. A generalization of the model to include arbitrary three-dimensional distribution of laminae in ‘quasi-plane strain’ is included. The effect of various flow rules adopted for plastic straining is indicated.     

Coping mechanisms practised by drought victims (1994/5) in North Bengal, Bangladesh

Droughts are recurrent features in Bangladesh, affecting plant growth and leading to loss of crop production, food shortages and, for many people, starvation. The main objective of this study is to examine the means by which residents of a drought-affected area of Bangladesh cope with this hazard. Data were collected during the summer of 1995 from 301 drought-affected households located in northwestern Bangladesh. Analysis suggests that respondent households practised an array of adjustments to mitigate adverse effects of the 1994/5 drought. While both high- and low-income households were affected by the drought, households belonging to the lower socioeconomic group suffered the most, receiving the least support from the national government. Government responses were delayed and inadequate in providing financial and other assistance to the drought victims. It is suggested that the government should be prepared for drought long before the occurrence of such an event.