Stable isotope geochemistry of Oxygen and Hydrogen: A case study of the Satluj River Basin, India  

2021 ◽  
Author(s):  
Akhtar Jahan ◽  
Mohd Usman Khan ◽  
Nachiketa Rai ◽  
Abhayanand Singh Maurya ◽  
Sudhir Kumar
Keyword(s):  
Stable Isotope ◽  
River Water ◽  
Water Samples ◽  
Hydrological Cycle ◽  
Indian Subcontinent ◽  
Monsoon Season ◽  
Isotope Analysis ◽  
Mean Value ◽  
Isotopic Analyses ◽  
The Mean

<p>Stable isotope analysis of hydrogen and oxygen is one of the important methods used to model the hydrological cycle. Oxygen and hydrogen isotopic investigation of river water, its tributaries, and groundwater of its catchment from the Satluj basin was undertaken to estimate the contributions of the main sources comprising discharge during major periods throughout a hydrologic year.</p><p>Estimation of the snow/glaciers melt contribution is also very important for tracing the sources and processes regulating the flow from the provenance and reservoirs in the context of global warming, for estimating flood flow, and for other water resource development activities in large parts of the Indian subcontinent. Water samples were collected during the non-monsoon season at increasing altitudes. In this work, in addition to stable isotopes, we also assessed the water quality using various physicochemical parameters and geochemistry of the water.</p><p>From isotopic analyses of river water samples, the mean value of the δ<sup>18</sup>O was found to be ~ -13‰, and the mean value of δD was found to be~ -85‰. For the samples from Satluj tributaries, the mean value of the δ<sup>18</sup>O was ~ -11‰, and the mean value of δD was ~ -69‰. A mean value of -8.4‰, was found based on the δ<sup>18</sup>O measurements of the groundwater samples, while the average δD value was found to be ~ -55‰.</p><p>For the mainstream and tributary, LWL, y = 8.2604x +20.208, and range of d-excess (>10‰) and y = 8.2079x + 22.182 and d-excess > 10‰ indicates a system recharged by sources of recycled moisture derived from continental sources in addition to monsoonal climates. For the groundwater data, the slope is 6.7, and d-excess ranges from 7‰ to 17‰. These observations are suggestive of the monsoonal source of Indian Ocean precipitation that has experienced significant evaporation during the non-monsoon season.</p><p>Our new data clearly shows that the surface water whether mainstream, tributary, and groundwater isotopes are homogenized from regional trends in precipitation, modified by evaporation, and are thus greatly influenced by latitude, elevation, and patterns of climate.</p><p> </p>

scholarly journals Physicochemical Analysis of Mymensingh Municipality Sewage Water and Old Brahmaputra River water

2018 ◽  
Vol 10 (2) ◽  
pp. 105-108
Author(s):  
M Uddin ◽  
S Talukder ◽  
MS Hossen ◽  
MT Hossain
Keyword(s):  
River Water ◽  
Water Samples ◽  
Oxygen Demand ◽  
Sewage Water ◽  
Physicochemical Analysis ◽  
Mean Value ◽  
Brahmaputra River ◽  
Acceptable Range ◽  
Irrigation Water Use ◽  
The Mean

The study was conducted to investigate the physicochemical properties of the Old Brahmaputra River and Sewage water in Mymensingh Municipality. To perform the study fifty samples were collected from five different stations from the river and surrounding sewage discharge points. The samples were analyzed to determine pH, Electrical Conductivity (EC), Total Dissolved Solids (TDS), Dissolved Oxygen (DO), Biological Oxygen Demand (BOD), Lead (Pb) and Cadmium (Cd). The mean value of pH was 7.1 and 6.8 for river and sewage water samples, respectively. Mean EC value was 183 μS/cm and 589.18 μS/cm for river and sewage samples, respectively signifies that EC of all samples were within the acceptable range. 66.32 ppm and 260.36 ppm were the mean TDS value for river and sewage samples, respectively indicates no harm to aquatic lives and irrigation water use. Mean DO and BOD values for river water samples were 4.21 mg/L and 6.02 mg/L, respectively. 3.08 mg/L and 9.98 mg/L were the mean DO and BOD values for sewage water samples, respectively implies that river water is usable for irrigation but sewage water is unfit for it. Mean Pb concentration for river and sewage water samples was 0.428 ppm and 0.467 ppm, respectively.J. Environ. Sci. & Natural Resources, 10(2): 105-108 2017

scholarly journals Effect of COVID-19 Lockdown on Metal Concentration in the Water Column of Asia’s Largest Coastal Lagoon

2021 ◽  
Author(s):  
Syed Hilal Farooq ◽  
Amrit Kumar Mishra ◽  
Sandip Kumar Muhakud ◽  
Prasannajit Acharya ◽  
Pradipta Ranjan Muduli ◽  
...  
Keyword(s):  
Metal Concentration ◽  
Water Samples ◽  
Monsoon Season ◽  
Physical Parameters ◽  
Chilika Lagoon ◽  
Post Monsoon ◽  
Post Monsoon Season ◽  
The Mean ◽  
The Impact ◽  
Mean Concentration

A complete halt on all anthropogenic activities and human movement due to COVID-19 lockdown has provided a great opportunity to assess the impact of human activities on coastal marine ecosystems. The current study assessed the concentration of the metals in water samples of the largest brackish water lagoon of Asia; the Chilika lagoon in the state of Odisha, India between pre-COVID-19 and post-COVID-19 lockdown scenarios. Monthly water samples (n=30 stations) from 0.3 m depth were collected from three sectors of the lagoon seasonally; pre-monsoon, monsoon, and post-monsoon. In addition to various physical parameters [pH, salinity, alkalinity, (DO) dissolved oxygen, (TDS) total dissolved solids, and (EC) electrical conductivity] the collected water samples were analysed for 18 trace metals (Al, As, Ba, Be, Cd, Co, Cr, Cu, Fe, Mn, Mo, Ni, Pb, Sr, Th, Tl, U, V). Most of the physical parameters showed a significant variation between pre-and post-COVID-19 scenarios, except for pH and DO. The concentration of five metals (Be, Cd, Co, Ni, and Pb) remained below detection limits in all water samples. The impact of COVID-19 lockdown on the concentration of the metal in the water samples was noticed along with the three sectors of the lagoon. However, eight metals (Al, As, Cr, Fe, Mn, Th, U, and V) were significantly different between the COVID-19 scenarios and the remaining five metals were not statistically significant. The mean concentration of Al, As, Fe, Th, and V were higher in the pre-COVID-19 scenarios, whereas only Cr and Mn were higher in the post-COVID-19 scenarios. The mean concentration of U was similar among both COVID-19 scenarios, even though there were seasonal and sectoral differences. The seasonal influence of riverine influx was more evident on metal concentration during the monsoon season, whereas the difference between sectors was more prominent during the post-monsoon season. An increased number of correlations between physical parameters and metal concentration were observed in the post-monsoon season and post-COVID-19 scenario. This study provides evidence that the imposition of COVID-19 lockdown reduced metal influx in the water column and improved the water quality of the Chilika lagoon. Our results can be used as baseline for metal concentration in surface waters of the lagoon.

Stable Isotopes

Anthropology ◽  
2016 ◽  
Author(s):  
Eric Bartelink
Keyword(s):  
Stable Isotopes ◽  
Stable Isotope ◽  
Stable Isotope Analysis ◽  
Hydrological Cycle ◽  
Tooth Enamel ◽  
Isotope Analysis ◽  
Serial Sections ◽  
Major Area ◽  
Travel History ◽  
Mineral Fraction

Stable isotope analysis refers broadly to a series of chemical methods used to study phenomena such as earth systems, the hydrological cycle, and ecology. The use of stable isotopes in anthropology traces its beginnings to the late 1970s. Originally focused on geological, hydrological, and ecological problems, stable isotope analysis now is a major component of the anthropologist’s toolkit. Current applications within anthropology draw from the core scientific disciplines but adapt these methods for specific research questions within archaeology, bioarchaeology, paleoanthropology, and forensic anthropology. One major area of study is dietary reconstruction, which focuses on isotope analysis of human skeletons to examine temporal and regional dietary patterns, as well as variation associated with sex, age, mortuary patterns, and social status. More specialized approaches examine weaning and childhood diet patterns using serial sections of tooth enamel and dentin. Another major area of isotope research in anthropology is the study of past residence patterns (e.g., migration and mobility). Some stable isotopes record information about the local water and geology, and thus provide information regarding the place of origin or travel history of an individual. By examining multiple isotopes in different tissues, anthropologists can reconstruct changes in residence patterns. For example, isotopes in enamel bioapatite (mineral fraction) do not change throughout life, so teeth provide a record of where a person lived when a particular tooth formed. Bone collagen (organic fraction) and bioapatite (mineral fraction), in contrast, are constantly replaced through remodeling; thus, if a person moved to a new geographic region, the isotope values in their bones will shift toward the new location over time. By comparing the isotopes in teeth versus bones, anthropologists can detect whether a person was local or nonlocal to the area where they died. In instances where hair or nails are preserved (e.g., mummies, modern forensic cases), serial sections of these tissues can be used to provide a detailed record of diet or travel history in the months prior to death. More recently, forensic anthropologists have begun to examine stable isotopes in modern human remains to aid with medicolegal identification. These methods are especially useful when a decedent is nonlocal to the area where they died (for example, a recent traveler or foreign-born individual).

An improved method for recovering and preconcentrating mercury in natural water samples for stable isotope analysis

2019 ◽  
Vol 34 (11) ◽  
pp. 2303-2313 ◽  
Author(s):  
Kai Li ◽  
Che-Jen Lin ◽  
Wei Yuan ◽  
Guangyi Sun ◽  
Xuewu Fu ◽  
...  
Keyword(s):  
Stable Isotope ◽  
Isotopic Composition ◽  
Stable Isotope Analysis ◽  
Natural Water ◽  
Water Samples ◽  
Isotope Analysis ◽  
New Method ◽  
Improved Method ◽  
Natural Water Samples

A new method is developed to meet the criteria for precise and efficient measurements of mercury isotopic composition in various water samples.

scholarly journals Seasonal variation and characterization of effluents of fertilizer factory

2015 ◽  
Vol 26 (2) ◽  
pp. 136-146
Author(s):  
K Fatima ◽  
MK Hossain ◽  
MA Islam
Keyword(s):  
Water Quality ◽  
Water Samples ◽  
Quality Parameters ◽  
Mean Value ◽  
Dry Season ◽  
Chemical Parameters ◽  
Wet Season ◽  
Physico Chemical ◽  
The Mean ◽  
Nitrite Nitrate

The study was carried out to assess the water quality of the Jamuna river affected by effluents discharged from the nearby Jamuna Fertilizer Company Limited and its temporal change over wet and dry seasons due to change of the physico-chemical parameters. Effluents of the factories and water samples were collected from four different selected stations during the period of June to August 2014 and January to March 2015.The results further revealed that the water samples showed a remarkable variation in physico-chemical parameters during the wet and dry season. In wet season the mean value of temperature, pH, EC, TDS, TSS, DO, BOD, ammonium, nitrite, nitrate and chloride were28.63± 3.79 °C, 8.10± 0.85, 664.41± 599.54µscm-1, 370.91± 111.38 ppm, 74.49± 25.90 ppm, 6.11 ± 1.28 ppm, 75.39 ± 140.86 ppm 296.74± 303.03 ppm, 12.31±21.38 ppm,  15.19±24.49 ppm and 15.23±8.72 ppm, respectively In the dry season the mean value of temperature, pH, EC, TDS, TSS, DO, BOD, ammonium, nitrite, nitrate and chloride were31.69 ±3.18°C, 8.44± 0.66, 786.25±551.18µscm1, 338.37± 94.70 ppm, 72.08± 58.83 ppm, 5.45 ± 0.95 ppm, 86.93 ± 159.82 ppm, 347.91± 291.60 ppm, 13.68±23.1 ppm, 18.34± 24.92 ppm and 18.3±9.32 ppm, respectively. The comparative study showed that most of the effluent and water quality parameters were higher in dry season than those of the wet season because in dry season less quantity of water remains in the river and in wet season more water remains in river that has great dilution capacity. For existence and conservation of aquatic resources, it is essential to investigate the water quality and surrounding environment of the river.Progressive Agriculture 26 (2): 136-146, 2015

Environmental change and seasonal behavior of mastodons in the Great Lakes region inferred from stable isotope analysis

2014 ◽  
Vol 82 (2) ◽  
pp. 366-377 ◽  
Author(s):  
Jessica Z. Metcalfe ◽  
Fred J. Longstaffe
Keyword(s):  
Stable Isotope ◽  
Great Lakes ◽  
Stable Isotope Analysis ◽  
Seasonal Variations ◽  
Sampling Methods ◽  
Tooth Enamel ◽  
Isotope Analysis ◽  
Seasonal Behavior ◽  
Isotopic Analyses ◽  
Mammut Americanum

AbstractWe investigate seasonal variations in the diet and drinking water of four Great Lakes mastodon (Mammut americanum) specimens using stable isotope analysis of serially sampled inner-enamel bioapatite structural carbonate (δ13Csc, δ18Osc), and previously published bulk analyses. Isotopic analyses and thin section measurements showed that mastodon tooth enamel extension rates (~ 12–4 mm/yr, decreasing toward the cervix) were lower than those of mammoths or modern elephants. Mastodons had distinct and highly regular seasonal variations in δ13Csc and δ18Osc, which we interpret in the context of local glacial history and vegetation changes. Seasonal variations in δ18O were large but variations in δ13C were small, and may have been obscured if coarser sampling methods than our inner-enamel sampling approach were used. Thus, our approach may be particularly useful for understanding relatively small seasonal changes in δ13C within C3 environments. The seasonal patterns, though not entirely conclusive, suggest that the Ontario mastodons did not migrate over very long distances. Rather, the climate and seasonal dietary patterns of mastodons within the region changed over time, from ~ 12,400 to 10,400 14C yr BP (~ 15,000 – 12,000 cal yr BP). Insights gained using these methods can contribute to a better understanding of megafaunal extinctions and Paleoamerican lifeways.

SEGUIN FORM BOARD TEST: A PROPOSAL FOR APPROPRIATE NORMS

2021 ◽  
pp. 16-22
Author(s):  
Roopesh B Nagaraj
Keyword(s):  
Scale Score ◽  
Indian Subcontinent ◽  
Mean Value ◽  
Ordinal Scale ◽  
Flynn Effect ◽  
Board Test ◽  
Hyperactive Children ◽  
The Mean ◽  
Iq Method ◽  
The Times

Seguin Form Board Test (SFB) is one of the popular tests of intelligence for children in the Indian subcontinent. It is a much sought-after test due to its simplicity, ease of administration and takes less than 10 minutes to arrive at an IQ score. Further, it elicits interest in children, is easy to score and can be administered to even shy, speech impaired, autistic spectrum and/or attention decit and hyperactive children. There are standard norms and to keep up with the Flynn effect, researchers are conducting studies to update normative data to keep up with the times. However, all the available norms in India with respect to SFB, follow incorrect practices, such as, using SFB for children older than 10 years; inappropriate processes, such as, using only the mean value and ignoring standard deviation; and erroneous way of converting interval scale score to ordinal scale score to arrive at the ratio IQ method. These errors have been existing for decades, despite the possibility of having better and appropriate norms that matches the deviation IQ. This article attempts to highlight the pitfalls of adopting the existing norms with appropriate examples and gures. Further, the article proposes a better and more appropriate norms to arrive at an IQ.

scholarly journals Hydrochemistry and Application of GIS in Groundwater Quality in Nagalapura Taluk, Bellary District, Karnataka, India

2021 ◽  
Vol 20 (5) ◽  
Author(s):  
Maradi Sangrama Nayaka ◽  
T. Suresh ◽  
S. Manjappa ◽  
B. Suresh
Keyword(s):  
Water Quality ◽  
Groundwater Quality ◽  
Water Samples ◽  
Geological Structure ◽  
Mean Value ◽  
Ionic Ratio ◽  
Wilcox Diagram ◽  
The Mean ◽  
Conservation Of Natural Resources ◽  
Bore Well

The assessment of groundwater quality is essential for the conservation of natural resources. Hence, this study aims to assess the hydrochemistry of groundwater in and around the Nagalapura Taluk in Bellary district, Karnataka, India. The groundwater quality variables are mapped using a Geographic Information System (GIS). For the hypothesis, the mean value of ten groundwater quality variables was obtained from 50 bore well samples (2016-2018). To assess the lead ions and type of water, the USSL, SAR, and Na% were measured. Ionic ratio and Gibbs graphs were used to demonstrate the chemical reactions in the water samples. ArcGIS was used for spatial analysis of the quality variables. The results showed the order of Cl- > SO42- > HCO3- with water types Na+-Cl- and Cl-, and the order of Na+ > Mg++ > Ca++ > K+ with Na+ and Mg++ as the dominant anion and cation, respectively. The hydrochemistry of groundwater is determined by the geological structure in 64 percent of the water samples examined. The Wilcox diagram shows that no-alkali exposure to the crops is expected. Forty one samples (82%) fit within the C3-S1 group; this category is fit for irrigational needs. Only 01 and 03 samples showed maximum SAR during two seasons like pre-monsoon and post-monsoon periods. The maps showed that groundwater in the selected sites is usually of higher quality, whereas the presence of dolomite indicates a reduction in water quality.

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