Abstract

During the 2016 pre-monsoon dry season, we undertook a systematic study of water quality, specifically fecal contamination of drinking water, in the Khumbu Valley, Sagarmatha National Park (SNP, Mt. Everest region) and SNP buffer zone, Nepal. Our goal was to quantify physical parameters (temperature, pH, conductivity and total dissolved solids), and the presence of fecal coliforms (E. coli and total coliforms) in drinking water and drinking water sources (predominately groundwater-fed springs). This data set will function as a baseline for access to potable water and further monitoring. Sample sites were selected based on primary use as a drinking water and/or drinking water source for each community. In general, there is little correlation between and physical parameters however, there are very weak correlations between total coliform data and increasing temperature, and decreasing elevation and pH. There does, however, appear to be a correlation between population (including tourist numbers) and both E. coli and total coliforms. Our study clearly indicates that the presence of bacterial indicators of fecal pollution during the dry season. Samples from the more populated, lower altitude areas had higher levels of E. coli and coliform bacteria. Importantly, drinking water that was stored in tanks or transported long distances had a much higher incidence of E. coli and total coliforms suggesting that a change in water handling practices might have an important impact on drinking water quality and population health.

Highlights

  • IntroductionThe southern slopes of Mt. Everest are situated in the Sagarmatha National Park (SNP; Figure 1), which are part of the Nepali Himalaya: between 27 ̊30'19"N to 27 ̊06'45"N latitude to 86 ̊30'53"E to 86 ̊99'08"E longitude, and covers 1148 sq km area

  • During the 2016 pre-monsoon dry season, we undertook a systematic study of water quality, fecal contamination of drinking water, in the Khumbu Valley, Sagarmatha National Park

  • The 2011 WHO (World Health Organization) guidelines for drinking water suggest that potable water should contain less than 600 mg/L total dissolved solids (TDS)

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Summary

Introduction

The southern slopes of Mt. Everest are situated in the Sagarmatha National Park (SNP; Figure 1), which are part of the Nepali Himalaya: between 27 ̊30'19"N to 27 ̊06'45"N latitude to 86 ̊30'53"E to 86 ̊99'08"E longitude, and covers 1148 sq km area. The SNP has been a national park since 1976 and became a World Natural Heritage Site in 1979. A buffer area (~275 sq km) was created in 2002 to enhance the protection of the World Natural Heritage Site and is known at SNP Buffer Zone. The SNP, the trekking route to Mt. Everest, is a prime destination for international tourists and their accompanying porters and guides (Salerno et al 2010a, 2010b). Similar to many protected areas around the globe, tourism is the primary source of local income, and as such has been extensively promoted (WTO, 2005; Salerno et al 2013), prompting the World Tourism Organization (2005) to declare that “tourism operations in protected areas need to be carefully planned, managed and monitored to ensure their long-term sustainability” (WTO, 2005)

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