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1.
Ahmad Sarfaraz Hasnain Syed Iqbal. Glacier Research Group School of Environmental Sciences Jawaharlal Nehru University New Delhi- India 《中国地质大学学报(英文版)》2001,12(1)
I-DtjcrONAlpine environment enjoys a distinct set of physicochemical conditions asl compared to other aqueous systems. Thehydrochemical characteristics of meltwater draining from thisenvironment are different from the other aqueous ecosystemsdue to their mountainous nature and extreme cold climatic conditions. The high concentration of various chemical constitu.ents in meltwater shows the intensive chemical weathering inthe basin. The rapid physical weathering due tO grinding actionof the gl… 相似文献
2.
Abdul Hameed Shahida Hasnain 《中国海洋湖沼学报》2005,23(4):433-441
Many unicellular cyanobacteria were isolated from different places： fields, ponds, polluted water, and soils from Muredkey and Kasur tannery areas, near Lahore, Pakistan. Different media like BG 11 medium, Bold Basal medium, Chu＇s # 10 medium and Gotham＇s medium, in standard forms and with slight variations of ingredients, and different pH, temperature and light regimes were checked for the optimum growth of the isolates. The isolation pro- cedure was repeated with different concentrations of chromium to select the resistant strains. These selected strains grew on chromium of the range 100-200 μg/ml in BG 11 medium. Cyanobacteria were maintained in solid and liquid media with/without shaking. Cyanobacterial strains were collected from natural habitats that were accompanied by a diversified group of organisms including bacteria, protozoan, and rotifers etc. In order to eliminate these agents termed as contaminants, we used several methods including phenol treatment, use of antibiotic and careful manual picking of unicellular cyanobacteria. Resistance of these strains against different heavy metals （ZnSO4, MnSO4, NiSO4, COCl2, Pb（NO3）3, CuSO4, HgCl2, AgNO3 and CdCl2） and antibiotics （erythromycin, streptomycin, kanamycin, chloramphenicol, neomycin） was evaluated. Optimum temperature was 30℃ with variable pH for the reduction of Cr^6＋ in to Cr^3＋ in majority of strains. 相似文献
3.
Linear and nonlinear propagation of dust drift waves are investigated in the presence of Cairns and Kappa distributed ion population and Boltzmannian electrons. It is found the frequency of the dust drift wave is greatest for the Cairns, intermediate for Kappa and the least for the Maxwellian distributed ions. Using the drift approximation, a nonlinear equation is derived for the dust drift shock waves which reduces to a Korteweg-de Vries-Burgers (KdVB)-like equation in the comoving frame of reference. The solution of the KdVB-like equation is obtained using the tanh method. It is found that the non-Maxwellian ion population, dust neutral collision frequency as well as the inverse dust density scale length inhomogeneity alter the propagation characteristics of the nonlinear dust drift shock waves. Interestingly, it is found that the non-Maxwellian ion population modifies the scale lengths over which the nonlinear structures are formed. The work presented here may be useful to understand the low frequency electrostatic shock waves in inhomogeneous dusty plasmas such as those found in planetary environments. 相似文献
4.
Gardezi Hasnain Xing Aiguo Bilal Muhammad Zhuang Yu Muhammad Shoaib Janjua Shahmir 《Landslides》2022,19(2):451-463
Landslides - On July 5, 2021, a catastrophic rock avalanche hit an area in the upper Naltar valley, located in northwestern Gilgit, Pakistan. The 14 Mm3 rock mass flowed down the hillslope and... 相似文献
5.
Water and bed sediment samples collected from the Damodar River and its tributaries were analysed to study elemental chemistry
and suspended load characteristics of the river basin. Na and Ca are the dominant cations and HCO3 is the dominant anion. The water chemistry of the Damodar River basin strongly reflects the dominance of continental weathering
aided by atmospheric and anthropogenic activities in the catchment area. High concentrations of SO4 and PO4 at some sites indicate the mining and anthropogenic impact on water quality. The high concentration of dissolved silica,
relatively high (Na+K)/TZ+ ratio (0.2–0.4) and low equivalent ratio of (Ca+Mg)/(Na+K) indicate that dissolved ions contribute significantly to the weathering
of aluminosilicate minerals of crystalline rocks. The seasonal data show a minimum ionic concentration in the monsoon season,
reflecting the influence of atmospheric precipitation on total dissolved solids contents. The suspended sediments show a positive
correlation with discharge and both discharge and suspended load reach their maximum value during the monsoon season. Kaolinite
is the mineral that is possibly in equilibrium with the water. This implies that the chemistry of the Damodar River water
favours kaolinite formation. The concentration of heavy metals in the finer size fraction (<37 μ m) is significantly higher
than the bulk composition. The geoaccumulation index values calculated for Fe, Mn, Zn, Ni and Cr are well below zero, suggesting
that there is no pollution from these metals in Damodar River sediments.
Received: 21 January 1998 · Accepted: 4 May 1998 相似文献
6.
Nuraddeen Muhammad Babangida Muhammad Raza Ul Mustafa Khamaruzaman Wan Yusuf Mohamed Hasnain Isa 《Hydrogeology Journal》2016,24(7):1821-1833
Nonlinear complex behavior of pore-water pressure responses to rainfall was modelled using support vector regression (SVR). Pore-water pressure can rise to disturbing levels that may result in slope failure during or after rainfall. Traditionally, monitoring slope pore-water pressure responses to rainfall is tedious and expensive, in that the slope must be instrumented with necessary monitors. Data on rainfall and corresponding responses of pore-water pressure were collected from such a monitoring program at a slope site in Malaysia and used to develop SVR models to predict pore-water pressure fluctuations. Three models, based on their different input configurations, were developed. SVR optimum meta-parameters were obtained using k-fold cross validation and a grid search. Model type 3 was adjudged the best among the models and was used to predict three other points on the slope. For each point, lag intervals of 30 min, 1 h and 2 h were used to make the predictions. The SVR model predictions were compared with predictions made by an artificial neural network model; overall, the SVR model showed slightly better results. Uncertainty quantification analysis was also performed for further model assessment. The uncertainty components were found to be low and tolerable, with d-factor of 0.14 and 74 % of observed data falling within the 95 % confidence bound. The study demonstrated that the SVR model is effective in providing an accurate and quick means of obtaining pore-water pressure response, which may be vital in systems where response information is urgently needed. 相似文献
7.
M. Ashraf M. Sc. M. S. S. Hasnain Ph.D. O. Berge Ph.D. 《International Journal of Environmental Science and Technology》2006,3(1):43-51
Effect of soil salinity on physico-chemical and biological properties renders the salt-affected soils unsuitable for soil microbial processes and growth of the crop plants. Soil aggregation around roots of the plants is a function of the bacterial exo-polysaccharides (EPS), however, such a role of the EPS-producing bacteria in the saline environments has rarely been investigated. Pot experiments were conducted to observe the effects of inoculating six strains of EPS-producing bacteria on growth of primary (seminal) roots and its relationship with saccharides, cations (Ca2+, Na+, K+) contents and mass of rhizosheath soils of roots of the wheat plants grown in a salt-affected soil. A strong positive relationship of RS with different root growth parameters indicated that an integrated influence of various biotic and abiotic RS factors would have controlled and promoted growth of roots of the inoculated wheat plants. The increase in root growth in turn could help inoculated wheat plants to withstand the negative effects of soil salinity through an enhanced soil water uptake, a restricted Na+ influx in the plants and the accelerated soil microbial process involved in cycling and availability of the soil nutrients to the plants. It was concluded that inoculation of the EPS-producing would be a valuable tool for amelioration and increasing crop productivity of the salt-affected soils. 相似文献
8.
This paper describes the geological, geotechnical and chemical properties of some Sabkha (lagoonal) soils in the Benghazi plain. Several buildings constructed on such soils show tilting and cracks. The cause of this trouble has been traced to the special characteristics of Sabkha soils. It is suggested that improved mix design and dense concrete should be used so as to make concrete in the foundation impermeable. 相似文献
9.
The distribution of Si, Al, Fe, Mn, Cu, Zn, Ni and Cr in different grain-size fractions and geochemical association of Fe,
Mn, Cu and Zn with <63-μm size fraction of bed sediments of Damodar River has been studied. In general, concentrations of
heavy metals tend to increase as the size fractions get finer. However at two sites, near mining areas, the coarser particles
show similar or even higher heavy metal concentrations than finer ones. The higher residence time and/or presence of coarser
particles from mining wastes are possibly responsible for higher metal content in the coarser size fractions. The chemical
fractionation study shows that lithogenic is the major chemical phase for heavy metals. Fe and Mn are the major elements of
the lithogenic lattice, constituting 34–63% and 22–59%, respectively, of total concentrations. Fe-Mn oxide and organic bound
fractions are significant phases in the non-lithogenic fraction. The carbonate fraction is less significant for heavy metal
scavenging in the present environment and shows the following order of abundance Zn>Cu>Mn>Fe. The exchangeable fraction of
the Damodar sediments contains very low amounts of heavy metals suggesting poor bioavailability of metals.
Received: 18 August 1998 · Accepted: 1 December 1998 相似文献
10.
The Alaknanda river, a major Himalayan proglacial stream, and its tributaries have been studied to evaluate sediment sources, production mechanisms, and transport pathways in the Alaknanda river basin. The study is based on a single-time sampling of the river and its tributaries and gives an insight into the suspended load pattern of the river from its source to its confluence with the other major Himalayan proglacial stream, the Bhagirathi. It is tentatively concluded that the suspended load of the Alaknanda is primarily due to natural processes and events and does not reflect the effects of human intervention. 相似文献