scholarly journals Support for the fluvial recharge model for arsenic contamination of groundwater in Pokhara Valley, Nepal Himalaya

2013 ◽  
Vol 46 ◽  
Author(s):  
Steven H. Emerman ◽  
Kevin L. Stuart ◽  
Ajit Sapkota ◽  
Sabina Khatri ◽  
Basanta Raj Adhikari ◽  
...  

Elevated levels of As in groundwater in the floodplain of the Ganges River have been well-documented over the past 15 years. Recent studies have shown that elevated groundwater As occurs even in Kathmandu Valley in Nepal, a tectonic valley well upstream of the floodplain of the Ganges River. Moreover, studies in Kathmandu Valley showed surface water As to be statistically indistinguishable from groundwater As, which led to the fluvial recharge model in which elevated groundwater As results from losing streams (streams that recharge groundwater) with elevated As, which is a consequence of rapid erosion caused by a combination of monsoon climate, tectonic uplift and deforestation. The objective of this study was to further test the fluvial recharge model and other existing models in Pokhara Valley, another tectonic valley in Nepal Himalaya far upstream from the floodplain of the Ganges River. In November 2010 water samples were collected from 20 hand-dug wells (depths 2-18 m), 12 borings (depths 34-220 m), four springs, 16 streams, three lakes and two caves. Arsenic concentrations in all but one of the 57 samples (a stream) exceeded the WHO As Standard (As= 0.01 mg/L). The As concentration of all surface water (geometric mean As = 0.067 mg/L) was statistically indistinguishable (P = 0.43) from that of all groundwater (geometric mean As = 0.086 mg/L), which is consistent with the fluvial recharge model. Groundwater As was uncorrelated with either sulfate or any combination of the transition elements, which is inconsistent with both the reductive-dissolution and sulfide-oxidation models.

2010 ◽  
Vol 40 ◽  
pp. 49-60 ◽  
Author(s):  
Steven H. Emerman ◽  
Tista Prasai ◽  
Ryan B. Anderson ◽  
Mallory A. Palmer

Elevated levels of arsenic (As) in groundwater in the flood plain of the Ganges River have been well-documented over the past decades. The objective of this study was to measure As and the transition elements normally associated with As in the Kathmandu Valley in Nepal, a heavily populated tectonic valley in the upper reaches of the Ganges River system. Water samples were collected from six shallow tubewells (depth < 50 m), eight deep tubewells and 13 dug wells and stone spouts. Electrical conductivity, temperature and pH were measured on-site and concentrations of As, Fe, Cu, Ni, Co, Mn, Zn and Cr were measured with a spectrophotometer. Five tubewells and four dug wells had As levels exceeding the Nepal Interim Standard (As = 0.05 mg/L). There was no statistically significant clustering of As levels either with depth or horizontal location. Arsenic was uncorrelated with either Fe (R2 = 0.096), Mn (R2 = 0.0004) or any combination of transition elements (R2 < 0.083), which is inconsistent with both the reduction-dissolution and the sulfide oxidation models for As release. The geometric mean As level of groundwater (As = 0.015 mg/L) was indistinguishable from the geometric mean As level of surface water (As = 0.013 mg/L) obtained from 48 river samples from the Kathmandu Valley in a previous study. We are suggesting that elevated groundwater As results not from subsurface redox conditions, but from losing streams with elevated As, which is a consequence of rapid erosion caused by a combination of monsoon climate, tectonic uplift and deforestation.


2014 ◽  
Vol 47 (1) ◽  
pp. 1-21 ◽  
Author(s):  
Steven H. Emerman ◽  
Janae R. Nelson ◽  
J. Kade Carlson ◽  
Tracy K. Anderson ◽  
Anusha Sharma ◽  
...  

Recent studies have shown that elevated groundwater as occurs even in Kathmandu and Pokhara Valleys in Nepal, two tectonic valleys well upstream of the floodplain of the Ganges River. Moreover, studies in both valleys showed surface water As to be statistically indistinguishable from groundwater As, which led to the fluvial recharge model in which elevated groundwater As results from losing streams with elevated As, which is a consequence of rapid erosion caused by a combination of monsoon climate, tectonic uplift and deforestation. The objective of this study was to further test the fluvial recharge model in Mustang Valley, the third major tectonic valley in Nepal Himalaya far upstream from the floodplain of the Ganges River. In May 2011 water samples were collected from 33 surface water sites (24 directly from streams and 9 from canals, pipes or taps fed by streams) and 24 groundwater sites (10 directly from springs and 14 from pipes or taps fed by springs). The WHO As Standard was exceeded in 47% of surface water samples and 79% of groundwater samples, including all nine functioning water taps in Lo-Manthang, the largest village. Separating samples into a high- As Region I (geometric mean As = 0.071 mg/L) and a low-As Region II (undetectable As for 85% of samples) showed that surface water As and groundwater As were statistically indistinguishable within each region. Only Region I receives overland flow from the exposed Mustang and Mugu Granites. The correspondence between groundwater As and watershed surface lithology is further evidence for the fluvial recharge model.


2021 ◽  
Author(s):  
Stefan Krause ◽  

&lt;p&gt;It is probably hard to overestimate the significance of the River Ganges for its spiritual, cultural and religious importance. As the worlds&amp;#8217; most populated river basin and a major water resource for the 400 million people inhabiting its catchment, the Ganges represents one of the most complex and stressed river systems globally. This makes the understanding and management of its water quality an act of humanitarian and geopolitical relevance. Water quality along the Ganges is critically impacted by multiple stressors, including agricultural, industrial and domestic pollution inputs, a lack and failure of water and sanitation infrastructure, increasing water demands in areas of intense population growth and migration, as well as the severe implications of land use and climate change. Some aspects of water pollution are readily visualised as the river network evolves, whilst others contribute to an invisible water crisis (Worldbank, 2019) that affects the life and health of hundreds of millions of people.&lt;/p&gt;&lt;p&gt;We report the findings of a large collaborative study to monitor the evolution of water pollution along the 2500 km length of the Ganges river and its major tributaries that was carried out over a six-week period in Nov/Dec 2019 by three teams of more than 30 international researchers from 10 institutions. Surface water and sediment were sampled from more than 80 locations along the river and analysed for organic contaminants, nutrients, metals, pathogen indicators, microbial activity and diversity as well as microplastics, integrating in-situ fluorescence and UV absorbance optical sensor technologies with laboratory sample preparation and analyses. Water and sediment samples were analysed to identify the co-existence of pollution hotspots, quantify their spatial footprint and identify potential source areas, dilution, connectivity and thus, derive understanding of the interactions between proximal and distal of sources solute and particulate pollutants.&lt;/p&gt;&lt;p&gt;Our results reveal the co-existence of distinct pollution hotspots for several contaminants that can be linked to population density and land use in the proximity of sampling sites as well as the contributing catchment area. While some pollution hotspots were characterised by increased concentrations of most contaminant groups, several hotspots of specific pollutants (e.g., microplastics) were identified that could be linked to specific cultural and religious activities. Interestingly, the downstream footprint of specific pollution hotspots from contamination sources along the main stem of the Ganges or through major tributaries varied between contaminants, with generally no significant downstream accumulation emerging in water pollution levels, bearing significant implications for the spatial reach and legacy of pollution hotspots. Furthermore, the comparison of the downstream evolution of multi-pollution profiles between surface water and sediment samples support interpretations of the role of in-stream fate and transport processes in comparison to patterns of pollution source zone activations across the channel. In reporting the development of this multi-dimensional pollution dataset, we intend to stimulate a discussion on the usefulness of large river network surveys to better understand the relative contributions, footprints and impacts of variable pollution sources and how this information can be used for integrated approaches in water resources and pollution management.&lt;/p&gt;


Chemosphere ◽  
2009 ◽  
Vol 76 (1) ◽  
pp. 55-62 ◽  
Author(s):  
Leo W.Y. Yeung ◽  
Nobuyoshi Yamashita ◽  
Sachi Taniyasu ◽  
Paul K.S. Lam ◽  
Ravindra K. Sinha ◽  
...  

2021 ◽  
Author(s):  
Holly Nel ◽  

&lt;p&gt;Twenty rivers have been estimated previously to account for almost 70% of global plastic emissions to the marine environment. Of these, the Ganges River was second only to the Yangtze River. Yet, scale and complexity of the Ganges River network make assessing microplastic contamination along the watercourse, including the attribution of suspected pollution sources challenging. Here we analyse post-monsoon spatial variation of microplastics along a 2500km length of the Ganges. River sediments and surface water were sampled during Nov/Dec 2019 at 81 locations that covered a variety of hydrological conditions, morphological attributes and land-use categories (e.g., downstream of large urban areas, rural areas with agriculture, major tributaries). Sediment samples were collected from the riverbank (waterline) and stored in glass jars while 100L water samples were filtered on-site through a 63&amp;#181;m sieve. Plastic particles between 63 and 5000&amp;#181;m were extracted by means of density separation followed by organic matter digestion with Fenton reagent. Extracts were subsequently stained with Nile red to improve detection of ambiguous particles. Physical and chemical properties such as shape, size, and polymer type where characterised using Fluorescence microscopy, Confocal Raman, and FT-IR imaging to understand differences along the river continuum. Our findings were analysed in relation to other key water quality parameters, various land-use descriptors and hydrogeomorphological characteristics, which allowed us to better understand the main drivers of microplastic transport and fate. Our survey results reveal an increasing downstream trend in sediment microplastic concentrations. The existence of distinct microplastic pollution hotspots in areas of high population density as well as areas of high cultural and spiritual relevance are detected. Interestingly, longitudinal concentration profiles in sediment and surface water samples do not match, hinting at differences in source attributions as well as transport, accumulation and long-term storage mechanisms, which is especially important in light of the variations seen in microplastic shape and size distribution patterns. Our results can be used as a springboard for future research assessing local microplastic contamination and aid in the refinement of medium and large-scale models estimating microplastic export.&lt;/p&gt;


1995 ◽  
Vol 25 (3) ◽  
pp. 192-196 ◽  
Author(s):  
G. J. Chakrapani ◽  
V. Subramanian ◽  
R. J. Gibbs ◽  
P. K. Jha

2013 ◽  
Vol 13 (3) ◽  
pp. 795-808 ◽  
Author(s):  
N. Sh. Chen ◽  
G. Sh. Hu ◽  
W. Deng ◽  
N. Khanal ◽  
Y. H. Zhu ◽  
...  

Abstract. The Kosi River is an important tributary of the Ganges River, which passes through China, Nepal and India. With a basin area of 71 500 km2, the Kosi River has the largest elevation drop in the world (from 8848 m of Mt Everest to 60 m of the Ganges Plain) and covers a broad spectrum of climate, soil, vegetation and socioeconomic zones. The basin suffers from multiple water related hazards including glacial lake outburst, debris flow, landslides, flooding, drought, soil erosion and sedimentation. This paper describes the characteristics of water hazards in the basin, based on the literature review and site investigation covering hydrology, meteorology, geology, geomorphology and socio-economics. Glacial lake outbursts are a huge threat to the local population in the region and they usually further trigger landslides and debris flows. Floods are usually a result of interaction between man-made hydraulic structures and the natural environment. Debris flows are widespread and occur in clusters. Droughts tend to last over long periods and affect vast areas. Rapid population increase, the decline of ecosystems and climate change could further exacerbate various hazards in the region. The paper has proposed a set of mitigating strategies and measures. It is an arduous challenge to implement them in practice. More investigations are needed to fill in the knowledge gaps.


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