Limestone is one of the essential raw materials in the cement,paint,steel,ceramic,glass,chemical,pharmaceutical,paper,and fertilizer industries.In India,only 8%of the limestone resources are placed under the reserve c...Limestone is one of the essential raw materials in the cement,paint,steel,ceramic,glass,chemical,pharmaceutical,paper,and fertilizer industries.In India,only 8%of the limestone resources are placed under the reserve category,of which 97%is of cement grade.Thus,India depends on imports to bridge the demand‐supply gap of steel,blast furnace,and chemical‐grade limestone.Efforts of Geological Survey of India(GSI)to locate alternate sources for limestone led to the discovery of enormous quantities of carbonate minerals called limemud from the continental shelf margin of the west coast of India.GSI carried out systematic studies to explore the nature of the disposition,quality,quantity,and suitability of the offshore limemud for various industrial applications.A preliminary estimate of resources using high‐resolution subbottom profiling and sediment core sample studies established the occurrence of more than 172 billion tonnes of high‐grade(The content of CaCO3 is greater than 80 wt%)limemud in 0.4–28.0m thick stratified sediment layers spread over an area of 18000 km2.Chemical,physical,mineralogical,beneficiation,and agglomeration studies found the offshore limemud as a potential replacement for limestone in the cement,filler,blast furnace,steel melting shop,lime production,paint,and Grade‐I steel industries.An assessment of mining and transportation costs indicates that the offshore limemud(USD 5–6/ton)is more cost‐effective than that imported from other countries(USD16‐18/ton).With several advantageous factors like low impurity,mode of occurrence in overburden‐free stratified form,fine‐grained slurry nature,and shallow water depth,sustainable mining of offshore limemud could be a future reality with controllable technological,economic,and environmental challenges.展开更多
A total of 103 surface sediment samples collected from the water depth range of 15-3300 m along Vijaydurg-Karwar stretch of central west coast of India were analyzed for foraminiferal content. Relict benthic foraminif...A total of 103 surface sediment samples collected from the water depth range of 15-3300 m along Vijaydurg-Karwar stretch of central west coast of India were analyzed for foraminiferal content. Relict benthic foraminiferal assemblage was noted within 50--135 m water depth. The relict benthic foraminiferal assemblage that includes Amphistegina, Operculina and Alveolinella in sediment samples within the water depth of 85-- 135 m indicates presence of coral reef at this depth during Early Holocene. The presence of barnacle fouling on Relict foraminifera at 60--90 m confirms the paleo-shoreline. The shallow depth zone is characterized by presence of agglutinated relict foraminifera. The agglutinated forms indicate freshwater influx, which eventually increased the sea level and subsequently deteriorated the paleo-coral reef.展开更多
Objective:To study the extent of undernutrition at district level and the socio-economic determinants of underweight children aged 0-71 months in West Bengal.Methods:The data were accessed from the Reproductive and Ch...Objective:To study the extent of undernutrition at district level and the socio-economic determinants of underweight children aged 0-71 months in West Bengal.Methods:The data were accessed from the Reproductive and Child Health Survey(RCHS-II),which contained information of 7 SSO children and their parents.Information of socio-economic variables about the associated families of these children had also been taken for our study.This study computed weight-for-age z-scores to assess the nutritional status of the children using WHO(2006) reference.Results:The prevalence of underweight varied over the districts.Districts with very high prevalence of underweight children were Murshidabad,Burdwan,Purulia,Medinipur, Howrah and South 24 Parganas.High prevalent districts for both boys and girls were Jalpaiguri and Coochbihar.Low prevalent districts for both boys and girls were South Dinajpur,Nadia and Kolkata.The percentage of underweight children were more in rural areas among Muslim families with illiterate parents and low standard of living.In Murshidabad,Bankura,Nadia, Medinipur and South 24 Parganas districts,i.e.,where prevalence of underweight children were higher,the rural and urban differences were less.The characteristics like religion,parents’ educational status and standard of living index showed significant effect on the children’s weights.Conclusions:Public intervention programs on the parent’s education and the standard of living of the households at district level should be given high priority to combat the children’s undernutrition problems so far as weight for age is concerned.展开更多
High resolution shallow seismic data was acquired from inner continental shelf of Goa,west coast of India to map underlying stratigraphic and buried geomorphic features of shelf strata.Seismic data revealed characteri...High resolution shallow seismic data was acquired from inner continental shelf of Goa,west coast of India to map underlying stratigraphic and buried geomorphic features of shelf strata.Seismic data revealed characteristic channel incisions beneath 4-15 m thick sediment layer and corresponds to multi cycle incisions.Stratigraphic analysis of these incision signatures reveals three prominent subaerial unconformities S6,S7 and S9.These unconformities were exposed during the last glacial,penultimate glacial(MIS-6)and prior to penultimate glacial(MIS-8)periods.On the basis of interpreted age of subaerial unconformities and differences in their morphological features,observed channel incisions have been divided grossly into three phases of incision.Phase-1 incisions are older than^330 kyr BP,whereas,incisions of Phase-2 and Phase-3 correspond to^320-125 kyr BP and^115-10 kyr BP respectively.Plan form of these incisions varied from a straight channel type to ingrown meander and then to anastomosing channel types.These channels meet at the confluence of present-day Mandovi and Zuari rivers.The confluence point has varied in due course of time because of cyclic incision and burial with repeated sea level fluctuations.The preserved main channel width varies from^100 m to 1000 m.and maximum channel depth reaches up to^35 m.Comparison of quantitative and qualitative morphologic results of different phases of incisions suggest that Phase-2 channels had^33%more mean bank full discharge than that of the Phase-3 channels.Phase-2 incisions had been carved in higher hydraulic energy condition as compared to Phase-3 incisions implying that the Indian summer monsoon was better during formative stages of Phase-2 incisions.展开更多
In Forster's masterpiece A Passage to India, the novelist deals in large parts with the contemporary Indian society under British rule and the complicated relations between the English and the native population. I...In Forster's masterpiece A Passage to India, the novelist deals in large parts with the contemporary Indian society under British rule and the complicated relations between the English and the native population. In this novel, Forster explores the difficulty to unify human relations,and exposes the eternal gaps between two nations. This paper will center on the eternal gaps of a Passage to India, which are represented by the misunderstandings between"India"and"British". By exploring and analyzing those gaps, the paper reaches the conclusion that those gaps can not be eliminated and the long-existing communication proposed by Forster is still a long way to go.展开更多
基金Geological Survey of India(Data collected as part of annual field programme of Geological Survey of India,Ministry of Mines,Government of India)。
文摘Limestone is one of the essential raw materials in the cement,paint,steel,ceramic,glass,chemical,pharmaceutical,paper,and fertilizer industries.In India,only 8%of the limestone resources are placed under the reserve category,of which 97%is of cement grade.Thus,India depends on imports to bridge the demand‐supply gap of steel,blast furnace,and chemical‐grade limestone.Efforts of Geological Survey of India(GSI)to locate alternate sources for limestone led to the discovery of enormous quantities of carbonate minerals called limemud from the continental shelf margin of the west coast of India.GSI carried out systematic studies to explore the nature of the disposition,quality,quantity,and suitability of the offshore limemud for various industrial applications.A preliminary estimate of resources using high‐resolution subbottom profiling and sediment core sample studies established the occurrence of more than 172 billion tonnes of high‐grade(The content of CaCO3 is greater than 80 wt%)limemud in 0.4–28.0m thick stratified sediment layers spread over an area of 18000 km2.Chemical,physical,mineralogical,beneficiation,and agglomeration studies found the offshore limemud as a potential replacement for limestone in the cement,filler,blast furnace,steel melting shop,lime production,paint,and Grade‐I steel industries.An assessment of mining and transportation costs indicates that the offshore limemud(USD 5–6/ton)is more cost‐effective than that imported from other countries(USD16‐18/ton).With several advantageous factors like low impurity,mode of occurrence in overburden‐free stratified form,fine‐grained slurry nature,and shallow water depth,sustainable mining of offshore limemud could be a future reality with controllable technological,economic,and environmental challenges.
文摘A total of 103 surface sediment samples collected from the water depth range of 15-3300 m along Vijaydurg-Karwar stretch of central west coast of India were analyzed for foraminiferal content. Relict benthic foraminiferal assemblage was noted within 50--135 m water depth. The relict benthic foraminiferal assemblage that includes Amphistegina, Operculina and Alveolinella in sediment samples within the water depth of 85-- 135 m indicates presence of coral reef at this depth during Early Holocene. The presence of barnacle fouling on Relict foraminifera at 60--90 m confirms the paleo-shoreline. The shallow depth zone is characterized by presence of agglutinated relict foraminifera. The agglutinated forms indicate freshwater influx, which eventually increased the sea level and subsequently deteriorated the paleo-coral reef.
文摘Objective:To study the extent of undernutrition at district level and the socio-economic determinants of underweight children aged 0-71 months in West Bengal.Methods:The data were accessed from the Reproductive and Child Health Survey(RCHS-II),which contained information of 7 SSO children and their parents.Information of socio-economic variables about the associated families of these children had also been taken for our study.This study computed weight-for-age z-scores to assess the nutritional status of the children using WHO(2006) reference.Results:The prevalence of underweight varied over the districts.Districts with very high prevalence of underweight children were Murshidabad,Burdwan,Purulia,Medinipur, Howrah and South 24 Parganas.High prevalent districts for both boys and girls were Jalpaiguri and Coochbihar.Low prevalent districts for both boys and girls were South Dinajpur,Nadia and Kolkata.The percentage of underweight children were more in rural areas among Muslim families with illiterate parents and low standard of living.In Murshidabad,Bankura,Nadia, Medinipur and South 24 Parganas districts,i.e.,where prevalence of underweight children were higher,the rural and urban differences were less.The characteristics like religion,parents’ educational status and standard of living index showed significant effect on the children’s weights.Conclusions:Public intervention programs on the parent’s education and the standard of living of the households at district level should be given high priority to combat the children’s undernutrition problems so far as weight for age is concerned.
基金financial support as JRF&SRF(Fellowship letter No.23/12/2012(ii)EU-V)
文摘High resolution shallow seismic data was acquired from inner continental shelf of Goa,west coast of India to map underlying stratigraphic and buried geomorphic features of shelf strata.Seismic data revealed characteristic channel incisions beneath 4-15 m thick sediment layer and corresponds to multi cycle incisions.Stratigraphic analysis of these incision signatures reveals three prominent subaerial unconformities S6,S7 and S9.These unconformities were exposed during the last glacial,penultimate glacial(MIS-6)and prior to penultimate glacial(MIS-8)periods.On the basis of interpreted age of subaerial unconformities and differences in their morphological features,observed channel incisions have been divided grossly into three phases of incision.Phase-1 incisions are older than^330 kyr BP,whereas,incisions of Phase-2 and Phase-3 correspond to^320-125 kyr BP and^115-10 kyr BP respectively.Plan form of these incisions varied from a straight channel type to ingrown meander and then to anastomosing channel types.These channels meet at the confluence of present-day Mandovi and Zuari rivers.The confluence point has varied in due course of time because of cyclic incision and burial with repeated sea level fluctuations.The preserved main channel width varies from^100 m to 1000 m.and maximum channel depth reaches up to^35 m.Comparison of quantitative and qualitative morphologic results of different phases of incisions suggest that Phase-2 channels had^33%more mean bank full discharge than that of the Phase-3 channels.Phase-2 incisions had been carved in higher hydraulic energy condition as compared to Phase-3 incisions implying that the Indian summer monsoon was better during formative stages of Phase-2 incisions.
文摘In Forster's masterpiece A Passage to India, the novelist deals in large parts with the contemporary Indian society under British rule and the complicated relations between the English and the native population. In this novel, Forster explores the difficulty to unify human relations,and exposes the eternal gaps between two nations. This paper will center on the eternal gaps of a Passage to India, which are represented by the misunderstandings between"India"and"British". By exploring and analyzing those gaps, the paper reaches the conclusion that those gaps can not be eliminated and the long-existing communication proposed by Forster is still a long way to go.
