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1.
In the present paper we have studied the resonance problem arising for critical mass values following Birkhoff's method of normalisation. It has been shown that for both the critical values the motion will remain unstable whether the critical terms are left in the Hamiltonian or carried to the coordinates in the process of normalisation. 相似文献
2.
In the present paper we have found the range of values of μ ande for the linear stability of the triangular points for the doubly photogravitational elliptic restricted problem of three
bodies. It has been shown that some resonances of the third and the fourth order exist which will need special investigation
for the determination of complete stability of the libration points under our terms of reference. 相似文献
3.
In the present paper we have studied the stability of the triangular libration points for the doubly photogravitational elliptic restricted problem of three bodies under the presence of resonances as well as under their absence. Here we have found the conditions for stability. 相似文献
4.
Ahmed Nasir Bodrud-Doza Md. Islam S. M. Didar-Ul Choudhry Manzoor Ahmad Muhib Md. Iftakharul Zahid Anwar Hossain Shahadat Moniruzzaman Md. Deb Nipa Bhuiyan Md. Abdul Quaiyum 《中国地球化学学报》2019,38(3):440-455
Acta Geochimica - To investigate the hydrogeochemical characteristics of groundwater 23 shallow, 30 intermediate and 38 deep wells samples were collected from Sylhet district of Bangladesh, and... 相似文献
5.
R. K. Choudhry 《Celestial Mechanics and Dynamical Astronomy》1977,16(4):411-419
In this paper the existence of collinear as well as equilateral libration points for the generalised elliptic restricted three body problem has been studied distinct from Kondurar and Shinkarik (1972) where a study has been made for the generalised circular restricted three body problem. Here the coordinates of the libration points have been found to be functions of timet. 相似文献
6.
M. Machendiranathan L. Senthilnathan R. Ranith A. Saravanakumar T. Thangaradjou S. B. Choudhry S. K. Sasamal 《中国海洋大学学报(英文版)》2016,15(6):1080-1086
The present study revealed proliferation of macro-algae modifying coral reef ecosystems in a different manner due to diseases and sedimentations in the Mandapam group of islands in the Gulf of Mannar. Benthic surveys were conducted with major attack of seven coral reefs diseases with high sedimentation rate, nine species of fleshy macro-algae(Turbinaria ornata, Turbinaria conaides, Caulerpa scalpelliformis, Caulerpa racemosa, Kappaphycus alvarezii, Padina gymnosphora, Sargassum wightii, Ulva reticulata and Calurpa lentillifera) proliferation against major corals life forms(Acropora branching, Acropora digitate, Acropora tabulate, coral massive, coral submassive, coral foliose and coral encrusting). The results confirm that diseased corals most favor to macro-algae growth(15.27%) rather than the sedimentation covered corals(8.24 %). In the degradation of coral life forms, massive corals were more highly damaged(7.05%) than any other forms. Within a short period of time(May to September), coral coverage shrank to 17.4% from 21.9%, macro-algae increased 23.51% and the average sedimentation rate attained 77.52 mg cm~(-2) d~(-1) with persisting coral reef diseases of 17.59%. The Pearson correlation showed that the coral cover decreased with increasing macro-algae growth, which was statistically significant(r =-0.774, n = 100, P 0.0005). The proliferation of the various macro-algae C. scalpellifrmis, T. ornata, C. racemosa, T. conaides, U. reticulata, S. wightii, K. alvarezii, P. gymnosphora and C. lentillifera increased with percentages of 6.0, 5.8, 5.7, 4.9, 4.2, 3.7, 2.7 and 1.9, respectively. If this trend continues, the next generation of new recruit corals will undoubtedly lead to a phase shift in Gulf of Mannar corals. 相似文献
7.
Sanjay Kumar Jain Sharad K. Jain V. Hariprasad Anju Choudhry 《Journal of the Indian Society of Remote Sensing》2011,39(2):259-270
Water balance of a basin involves estimation of input precipitation, runoff, infiltration and evapotranspiration (ET). Although
ET may have large variations over a big basin, it is commonly estimated using a few point measurements and this makes the
estimation error prone. Satellite based remote sensing data provides few parameters for estimation of energy fluxes, at the
land surface and atmosphere interaction in a distributed manner using the meteorological parameters. These parameters through
surface energy balance equation have been used for the estimation of ET in this study. Various spatially distributed variables
required for ET estimation; viz. NDVI, surface albedo, surface temperature etc. have been derived using remote sensing and
ancillary data for Tapi basin located in western India. Beside this field data such as rainfall, air temperature, relative
humidity, sunshine hours etc. have been used. For computation of runoff, Soil Conservation Services (SCS) approach has been
considered. Tapi basin up to Ukai dam has been selected as the study area. Satellite data from National Oceanic and Atmospheric
Administration (NOAA), Polar Orbiting Environmental Satellite, which carries the Advanced Very High Resolution Radiometer
(AVHRR), have been used for preparation of various maps required for runoff and ET analysis. The results of runoff and ET
have been compared with observed data for 2 years, 2002–2003 and the results have been found in good agreement with observed
data. 相似文献
8.
Pradeep K. Aggarwal Luis Araguas‐Araguas Manzoor Choudhry Michel van Duren Klaus Froehlich 《Ground water》2014,52(1):20-24
Uptake of atmospheric CO2 during sample collection and analysis, and consequent lowering of estimated ages, has rarely been considered in radiocarbon dating of groundwater. Using field and laboratory experiments, we show that atmospheric CO2 can be easily and rapidly absorbed in hyperalkaline solutions used for the extraction of dissolved inorganic carbon, resulting in elevated 14C measurements. Kinetic isotope fractionation during atmospheric CO2 uptake may also result in decrease of δ13C, leading to insufficient corrections for addition of dead carbon by geochemical processes. Consequently, measured 14C values of groundwater should not be used for age estimation without corresponding δ13C values, and historical 14C data in the range of 1 to 10% modern Carbon should be re‐evaluated to ensure that samples with atmospheric contamination are recognized appropriately. We recommend that samples for 14C analysis should be collected and processed in the field and the laboratory without exposure to the atmosphere. These precautions are considered necessary even if 14C measurements are made with an accelerator mass spectrometer. 相似文献
9.
Hydro power schemes operating in a free electricity market seek to maximize profits by differing generation rates to take best advantage of fluctuating selling prices, subject to the constraints of keeping storage lakes within their operational bounds and avoiding spillage losses. Various computer algorithms can be used in place of manual scheme operation to aid this maximization process, so it is desirable to quantify any profit gained from a given algorithm. A standard approach involves applying the algorithm to a period of past river flow records to see how much additional scheme income might have been obtained. This process requires the use of a hydro power scheme model, which inevitably can only approximate operational details, so the anticipated income gains are likely to be biased estimates of actual income gained from implementation of the algorithm. In addition to preliminary algorithm evaluation, it is desirable that hydro scheme managers have methodology to confirm anticipated income gain. Such confirmation can be difficult because true income gains are typically in the order of a few percentage and may not be easily distinguishable from background noise. We develop an approach, which allows estimation of true income gain for the situation where a change is made from manual to computer control of hydro power scheme operations, or upgrading from one maximization algorithm to another. The method uses a regression model to describe the former period of scheme operation. Postimplementation residuals from the regression predictions then provide estimates of actual income gain. The method can be sensitive to small but consistent income gains. Also, there is no requirement to construct any hydro scheme simulation model so bias effects should be considerably reduced. The approach was developed in the context of evaluating an income-maximization algorithm applied to a small hydro power scheme in the Kaimai Ranges of New Zealand. However, the methodology seems sufficiently simple and general to be applicable, with modification, to other power schemes moving toward increasing income through operational changes. 相似文献
10.
Nasir Ahmed Md.Bodrud-Doza S.M.Didar-Ul Islam Manzoor Ahmad Choudhry Md.Iftakharul Muhib Anwar Zahid Shahadat Hossain Md.Moniruzzaman Nipa Deb Md.Abdul Quaiyum Bhuiyan 《Acta Geochimica》2019,(3):440-455
To investigate the hydrogeochemical characteristics of groundwater 23 shallow, 30 intermediate and 38 deep wells samples were collected from Sylhet district of Bangladesh, and analyzed for temperature, pH, Eh, EC,DO, DOC, Na^+, K^+, Ca2+, Mg2+, Cl^-, SO_42-, NO_3^-,HCO_3^-, SiO_2^-, Fe, Mn and As. Besides, 12 surface water samples from Surma and Kushiyara Rivers were also collected and analyzed to understand the influence into aquifers. Results revealed that, most of the groundwater samples are acidic in nature, and Na–HCO_3 is the dominant groundwater type. The mean value of temperature, EC,Na^+, K^+, Ca2+, Mg2+, Cl^-, NO_3^- and SO_42- were found within the range of permissible limits, while most of the samples exceeds the allowable limits of Fe, Mn and As concentrations. However, relatively higher concentration of Fe and Mn were found in deep water samples and reverse trend was found in case of As. The mean concentrations of As in shallow, intermediate and deep wells were 39.3, 25.3and 21.4 lg/L respectively, which varied from 0.03 to148 lg/L. From spatial distribution, it was found that Fe,Mn and As concentrations are high but patchy in northern,north-western, and south-western part of Sylhet region. The most influential geochemical process in study area were identified as silicate weathering, characterized by active cation exchange process and carbonate weathering, which thereby can enhance the elemental concentrations in groundwater. Pearson's correlation matrix, principal component analysis and cluster analysis were also employed to evaluate the controlling factors, and it was found that, both natural and anthropogenic sources were influencing the groundwater chemistry of the aquifers. However, surface water has no significant role to contaminate the aquifers,rather geogenic factors affecting the trace elemental contamination. Thus it is expected that, outcomes of this study will provide useful insights for future groundwater monitoring and management of the study area. 相似文献