Scanning sky monitor (SSM) onboard AstroSat     

M. C. Ramadevi  S. Seetha  Dipankar Bhattacharya  B. T. Ravishankar  N. Sitaramamurthy  G. Meena  M. Ramakrishna Sharma  Ravi Kulkarni  V. Chandra Babu  Kumar  Brajpal Singh  Anand Jain  Reena Yadav  S. Vaishali  B. N. Ashoka  Anil Agarwal  K. Balaji  G. Nagesh  Manoj Kumar  Dhruti Ranjan Gaan  Prashanth Kulshresta  Pankaj Agarwal  Mathew Sebastian  A. Rajarajan  D. Radhika  Anuj Nandi  V. Girish  Vivek Kumar Agarwal  Ankur Kushwaha  Nirmal Kumar Iyer 《Experimental Astronomy》2017,44(1):11-23

Scanning Sky Monitor (SSM) onboard AstroSat is an Xray sky monitor in the soft X-ray band designed with a large field of view to detect and locate transient X-ray sources and alert the astronomical community about interesting phenomena in the X-ray sky. SSM comprises position sensitive proportional counters with 1D coded mask for imaging. There are three detector units mounted on a platform capable of rotation which helps covering about 50% of the sky in one full rotation. This paper discusses the elaborate details of the instrument and few immediate results from the instrument after launch.  相似文献   

The Cadmium Zinc Telluride Imager on AstroSat     

V. Bhalerao  D. Bhattacharya  A. Vibhute  P. Pawar  A. R. Rao  M. K. Hingar  Rakesh Khanna  A. P. K. Kutty  J. P. Malkar  M. H. Patil  Y. K. Arora  S. Sinha  P. Priya  Essy Samuel  S. Sreekumar  P. Vinod  N. P. S. Mithun  S. V. Vadawale  N. Vagshette  K. H. Navalgund  K. S. Sarma  R. Pandiyan  S. Seetha  K. Subbarao 《Journal of Astrophysics and Astronomy》2017,38(2):31

The Cadmium Zinc Telluride Imager (CZTI) is a high energy, wide-field imaging instrument on AstroSat. CZTI’s namesake Cadmium Zinc Telluride detectors cover an energy range from 20 keV to \(>200\) keV, with 11% energy resolution at 60 keV. The coded aperture mask attains an angular resolution of 17\(^\prime \) over a 4.6\(^\circ \) \(\times \) 4.6\(^\circ \)  (FWHM) field-of-view. CZTI functions as an open detector above 100 keV, continuously sensitive to GRBs and other transients in about 30% of the sky. The pixellated detectors are sensitive to polarization above \(\sim \)100 keV, with exciting possibilities for polarization studies of transients and bright persistent sources. In this paper, we provide details of the complete CZTI instrument, detectors, coded aperture mask, mechanical and electronic configuration, as well as data and products.  相似文献   

Study of high energy phenomena from near space using low-cost meteorological balloons     

Sandip K. Chakrabarti  Ritabrata Sarkar  Debashis Bhowmick  Arnab Bhattacharya 《Experimental Astronomy》2017,43(3):311-338

Indian Centre for Space Physics has taken a novel strategy to study low energy cosmic rays and astrophysical X-ray sources which involve very light weight payloads up to about five kilograms on board a single or multiple balloons which are used for meteorological purposes. The mission duration could be anywhere from 3-12 hours. Our strategy provides extreme flexibility in mission preparation and its operation using a very economical budget. There are several limitations but our innovative approach has been able to extract significant amount of scientific data out of these missions. So far, over one hundred missions have been completed by us to near space and a wealth of data has been collected. The payloads are recovered and are used again. Scientific data is stored on board computer and the atmospheric data or payload location is sent to ground in real time. Since each mission is different, we present here the general strategy for a typical payload and provide some results we obtained in some of these missions.  相似文献   

Bearing capacity of two interfering strip footings from lower bound finite elements limit analysis     

Jyant Kumar  Paramita Bhattacharya 《国际地质力学数值与分析法杂志》2013,37(5):441-452

A rigorous lower bound solution, with the usage of the finite elements limit analysis, has been obtained for finding the ultimate bearing capacity of two interfering strip footings placed on a sandy medium. Smooth as well as rough footing–soil interfaces are considered in the analysis. The failure load for an interfering footing becomes always greater than that for a single isolated footing. The effect of the interference on the failure load (i) for rough footings becomes greater than that for smooth footings, (ii) increases with an increase in ?, and (iii) becomes almost negligible beyond S/B > 3. Compared with various theoretical and experimental results reported in literature, the present analysis generally provides the lowest magnitude of the collapse load. Copyright © 2011 John Wiley & Sons, Ltd.  相似文献   

亚致死剂量铜对文昌鱼和玫瑰无须的组织病理学影响     

韩莉  郭斌 《中国海洋大学学报(自然科学版)》2008,38(1):95-102

采用半静水实验法测试研究了重金属Cu2 对文昌鱼(Branchiostoma belcheri)和玫瑰无须(Puntius conchonius)的急性致死毒性和亚急性毒性.实验结果表明,Cu2 对文昌鱼和玫瑰无须 24,48,72,96 h的半致死浓度分别为0.561,0.373,0.261,0.211 mg/L及0.976,0.783,0.562,0.473 mg/L,其安全质量浓度分别为0.021和0.047 mg/L.亚急性毒性实验中,文昌鱼和玫瑰无须 分别用浓度为20%和30%的 96 h LC50的Cu2 处理.不同器官的组织病理学观察结果表明,过量Cu2 对玫瑰无须 的鳃、肝脏、肾脏等器官产生毒害,对文昌鱼鳃和肝盲囊细胞也产生了严重的毒害,表现为细胞空泡化等明显的结构破坏.实验结果显示文昌鱼的肝盲囊和脊椎动物的肝脏一样,也是受过量铜显著毒害的主要靶器官器官.因此,文昌鱼的肝盲囊至少在经受过量Cu2 毒害方面与脊椎动物肝脏具有相似性,从生理功能方面为类文昌鱼祖先的盲囊(digestive caecum)是脊椎动物肝脏的前体这一假说提供了资料.  相似文献   

Concentration of polybrominated diphenyl ethers (PBDEs) in sediment cores of Sundarban mangrove wetland, northeastern part of Bay of Bengal (India)   总被引：4，自引：0，他引：4  

Binelli A  Sarkar SK  Chatterjee M  Riva C  Parolini M  Bhattacharya BD  Bhattacharya AK  Satpathy KK 《Marine pollution bulletin》2007,54(8):1220-1229

The paper presents the first comprehensive survey of congener profiles (12 congeners) of polybrominated diphenyl ethers (PBDEs) in core sediment samples (<63 microm) covering seven sites in Sundarban mangrove wetland (India). Gas-chromatographic analyses were carried out in GC-Ms/Ms for tri- to hepta- brominated congeners. Results pointed out a non-homogenous contamination of the wetland with summation operator(12) PBDE values ranging from 0.08 to 29.03 ngg(-1), reflecting moderate to low contamination closely in conformity to other Asian aquatic environments. The general order of decreasing congener contribution to the total load was: BDE 47>99>100>154, similar to the distribution pattern worldwide. Although tetrabromodiphenyl ether BDE 47 was found in all samples followed by hexabromodiphenyl ether BDE-154, they were not necessarily the dominant congeners. No uniform temporal trend on PBDE levels was recorded probably due to particular hydrological characteristics of the wetland and/on non-homologous inputs from point sources (untreated municipal wastewater and local industries, electronic wastes from the dump sites, etc.) of these compounds. Because of the propensity of PBDEs to accumulate in various compartments of wildlife and human food webs, evaluation of biological tissues should be undertaken as a high priority.  相似文献   

Characterisation of recharge processes and groundwater flow mechanisms in weathered-fractured granites of Hyderabad (India) using isotopes   总被引：4，自引：1，他引：3  

B. S. Sukhija  D. V. Reddy  P. Nagabhushanam  S. K. Bhattacharya  R. A. Jani  Devender Kumar 《Hydrogeology Journal》2006,14(5):663-674

In order to address the problem of realistic assessment of groundwater potential and its sustainability, it is vital to study the recharge processes and mechanism of groundwater flow in fractured hard rocks, where inhomogeneties and discontinuities have a dominant role to play. Wide variations in chloride, δ¹⁸O and ¹⁴C concentrations of the studied groundwaters observed in space and time could only reflect the heterogeneous hydrogeological setting in the fractured granites of Hyderabad (India). This paper, based on the observed isotopic and environmental chloride variations of the groundwater system, puts forth two broad types of groundwaters involving various recharge processes and flow mechanisms in the studied granitic hard rock aquifers. Relatively high ¹⁴C ages (1300 to ～6000 yr B.P.), δ¹⁸O content (?3.2 to ?1.5‰) and chloride concentration (<100 mg/l) are the signatures that identified one broad set of groundwaters resulting from recharge through weathered zone and subsequent movement through extensive sheet joints. The second set of groundwaters possessed an age range Modern to ～1000 yr B.P., chloride in the range 100 to ～350 mg/l and δ¹⁸O from ?3.2 to +1.7‰. The δ¹⁸O enrichment and chloride concentration, further helped in the segregation of the second set of groundwaters into three sub-sets characterized by different recharge processes and sources. Based on these processes and mechanisms, a conceptual hydrogeologic model has evolved suggesting that the fracture network is connected either to a distant recharge source or to a surface reservoir (evaporating water bodies) apart from overlying weathered zone, explaining various resultant groundwaters having varying ¹⁴C ages, chloride and δ¹⁸O concentrations. The surface reservoir contribution to groundwater is evaluated to be significant (40 to 70%) in one subset of groundwaters. The conceptual hydrogeologic model, thus evolved, can aid in understanding the mechanism of groundwater flow as well as migration of contaminants to deep groundwater in other fractured granitic areas.  相似文献   

Soft-sediment deformation structures from an ice-marginal storm–tide interactive system,Permo-Carboniferous Talchir Formation,Talchir Coalbasin,India     

H.N. Bhattacharya  Biplab Bhattacharya 《Sedimentary Geology》2010,223(3-4):380-389

Permo-Carboniferous Talchir Formation, Talchir Coalbasin, India, records sedimentation during a phase of climatic amelioration in an ice-marginal storm-affected shelf. Evidences of subtidal processes are preserved only under thick mud drapes deposited during waning storm phases. Various soft-sediment deformation structures in some sandstone/siltstone–mudstone interbeds, like syn-sedimentary faults, deformed laminations, sand–silt flows, convolute laminations and various flame structures, suggest liquefaction and fluidization of the beds due to passage of syn-depositional seismic shocks. In the Late Paleozoic ice-marginal shelf, such earthquake tremors could be generated by crustal movements in response to glacioisostatic adjustments of the basin floor.  相似文献   

A reappraisal of polymetamorphism in the Eastern Ghats belt — A view from north of the Godavari rift     

A. Bhattacharya  S. Gupta 《Journal of Earth System Science》2001,110(4):369-383

Evidence collated from different parts of the Eastern Ghats belt north of the Godavari rift (barring the “Western Charnockite Zone” ) indicates that this sector evolved through a series of compressive structures (F₁ to F₃), with prolific migmatization in quartzofeldspathic and metapelitic gneisses synchronous with F₁ shortening, as was the syn-F₁ emplacement of profuse megacrystic K-feldspar-bearing granitoid bodies. Thereafter, melt productivity of the rocks (synchronous withF ₂– F₃ folding) sharply decreased. Mineral parageneses stable in the S₁, S₂ and S₃ fabrics indicate persistence of granulite facies conditions. P-T estimates on orthopyroxene + garnet + plagioclase + quartz assemblages anchored to recrystallized mosaic that overgrow all penetrative fabric elements in mafic granulites, granitoids and quartzofeldspathic gneisses are in the range of 900‡-950‡C and P≅ 8–9 kbar. This estimate is comparable to those retrieved from sapphirine-bearing paragenesis in Mg-Al metapelites that appear to be diachronous in relation to the fabric elements, and arguably disrupt the granoblastic mosaic. These facets in the northern sector of the orogenic belt are compatible with either a single cycle of tectonic events (i.e., F₁, F₂ and F₃ in continuum), or temporally-separate thermo-tectonic events, with the peak of earlier metamorphism (pre- to syn-F₁) at lower temperature (in the granulite facies) in comparison to the record of high post-F₃-T_max values. It is suggested on the basis of the above evidence that the late Proterozoic/Pan-African granulites in the Eastern Ghats belt north of the Godavari rift, are unlikely to be reworked equivalents of any older granulitic crust, such as the ∼1.6 Ga granulites south of the rift. Instead, the temporally disparate sectors may represent different crustal segments with unconnected pre-amalgamation tectonic history. However, if the ∼ 1.6 Ga granulites of the Western Charnockite Zone continue northwards across the rift, as suggested by recent isotope data, there are serious doubts as to the validity of a north-south division within the Eastern Ghats belt.  相似文献   

Prediction equation for sand in Western Varanasi district,U.P., India     

Bireswar Bhattacharya 《Pure and Applied Geophysics》1971,85(1):290-297

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