Abstract

In 2014 we began the first systematic study of water quality, specifically fecal contamination of drinking water in the Khumbu Valley, Sagarmatha National Park (SNP, Mt. Everest region), Nepal. Our goal was to identify coliform bacteria and E. coli in drinking water and groundwater-fed springs to generate a data set that will function as a base for potable water supplies and further monitoring. Sampling occurred in May (pre-monsoon summer) and early November (post-monsoon early winter) 2014. Sample sites were selected based on proximity to villages and primary use as a drinking water source. Overall, the data presented a predictable correlation between fecal contamination and both elevation and increasing population/tourist traffic. Drinking water within the study area met current World Health Organization drinking water standards for the physical properties of temperature (2.8°C - 13°C), pH (5.27 - 7.24), conductivity (14.5 - 133 mS) and TDS (7.24 - 65.5 ppm). Samples from the more populated, lower altitude areas had higher levels of E. coli. Samples collected and analyzed in May (pre-monsoon summer) had a higher level of E. coli and coliform bacteria than samples collected in November (post-monsoon early winter) suggesting a seasonal dependence overlaid on the population signature. Surface water typically had higher E. coli values than groundwater-fed springs. Temperature, total dissolved solids and conductivity generally decreased with increasing elevation, whereas pH increased with increasing elevation. There appears to be significant presence of fecal contamination of water sources due to a combination of tourism, elevation and seasons.

Highlights

  • The Sagarmatha National Park (SNP; Figure 1) is located in the southeastern part of the Nepali Himalaya on theHow to cite this paper: Nicholson, K., Hayes, E., Neumann, K., Dowling, C. and Sharma, S. (2016) Drinking Water Quality in the Sagarmatha National Park, Nepal

  • Samples were taken from local drinking water sources. 3.1

  • With the exception of the Tengboche sample, both sets of our data compare well to Ghimire et al [5] who analyzed 51 sample locations on the four major rivers (DudhKoshi, ImjaKhola, BhoteKoshi, LobucheKhola (Figure 1)) within the SNP that showed an average temperatures varying between 8 ̊C and 13 ̊C, with an average of 10.7 (±1.5) ̊C, over three years

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Summary

Introduction

The Sagarmatha National Park (SNP; Figure 1) is located in the southeastern part of the Nepali Himalaya on theHow to cite this paper: Nicholson, K., Hayes, E., Neumann, K., Dowling, C. and Sharma, S. (2016) Drinking Water Quality in the Sagarmatha National Park, Nepal. The Sagarmatha National Park (SNP; Figure 1) is located in the southeastern part of the Nepali Himalaya on the. (2016) Drinking Water Quality in the Sagarmatha National Park, Nepal. The SNP is in the Solukhumbu district, approximately 140 km due east of Kathmandu and covers 1148 sq km. It ranges between 27 ̊30'19"N to 27 ̊06'45"N latitude to 86 ̊30'53"E to 86 ̊99'08"E longitude. The elevation of townships and communities in the SNP watersheds varies from 2610 m (Phakding) to over 5000 m at Mt. Everest base camp (EBC). The area experiences a temperate climate characterized by cold winters, warm summers and clear seasonality, with average annual precipitation ranging from 450 mm at EBC to 1800 mm at Lukla township (the town where tourists begin their trekking adventures). The Himalayan Mountains are the source of water for over a billion people and form the main headwaters for major river systems, such as the Ganges, Yangtze and Indus Rivers [1]

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