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High-Altitude Air Pollutants Monitored from Rainwater Chemistry in the Central Himalaya

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Abstract

Based on the ion chromatography method, the chemical characterization of rainwater (RW) samples collected over Srinagar (a location in central Himalaya) has been done during monsoon 2016 (MON-2016). The rainwater shows near acidic pH values ranging from 5.1 to 6.2 (average, 5.7 ± 0.6) during the study. The average ionic concentrations of 97 ± 10 μeq/1 were reported during MON-2016. Ca2+ has significantly high contribution of 24% as compared to NH4+ (18%), Na+ (9%), K+ (4%), and Mg2+ (3%) among cations, whereas Cl, SO42−, and NO3 have contribution of ~ 15, 11, and 7%, respectively, among anions during chemical analysis. We have reported SO42−/NO3 ratio as 1.49, which shows contribution of 60 and 40% from SO42− and NO3 ions within the predicted limit of RW (H2SO4, 60–70%, and HNO3, 30–40%). Ca2+, Mg2+, and NH4+ have neutralization factors as 2.51, 0.37, and 2.01, respectively, due to the neutralization of acidic species in RW. The non-sea salt (NSS) contribution to total Ca2+, K+, and Mg2+ indicates the major contribution from crustal origin, whereas the NSS contribution to the total Cl and SO42− was from the anthropogenic source. The principle component analysis (PCA) indicates that the first factor (i.e., natural sources, mainly dust and sea salts) has only ~ 9% variance. In contrast, the second factor (i.e., fossil fuel and biomass burning) has ~ 17% variance, and the third factor has 27% variance may be due to soil, agricultural, and biomass burning origin. The rest of the contributions are from mixed emission sources as well as by the transport of polluted air mass from the Indo-Gangetic Plain (IGP) and Punjab Rajasthan, Pakistan, and Afghanistan. This manuscript helps to understand the impact of crustal and anthropogenic sources in rainwater over the central Himalaya region of Uttarakhand.

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Abbreviations

AMBT:

Air mass back trajectory

APs:

Air pollutants

AWS:

Automatic weather station

EC:

Electrical conductivity

EF:

Enrichment factor

EIR:

Equivalent ionic ratio

FSI:

Forest Survey of India

HNBGU:

Hemwati Nandan Bahuguna Garhwal University

HYSPLIT:

Hybrid Single-Particle Lagrangian Integrated Trajectory

IGP:

Indo-Gangetic Plain

LRT:

Long-range transport

MON:

Monsoon

NF:

Neutralization factor

NH:

National highway

NOAA:

National Oceanic and Atmospheric Administration

NSS:

Non-sea salt

NSSF:

Non-sea salt fraction

PCA:

Principle component analysis

PCC:

Pearson correlation coefficient

PSCF:

Potential source contribution function

RW:

Rainwater

SS:

Sea salt

SSF:

Sea salt fraction

SW:

Seawater

VWM:

Volume-weighted mean

WMO:

World Meteorological Organization

WOA:

Weak organic acids

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Acknowledgements

The authors are thankful to the Director, IITM, for their guidance and unstinted support for this study. ASG thanks Prof Annpurna Nautiyal, Vice-Chancellor, HNBGU, Srinagar, Garhwal Uttarakhand, Head, Department of Physics, HNBGU, Srinagar, for encouragement and providing the necessary infrastructure facility for this study.

Funding

The authors are grateful to the Ministry of Earth Sciences (Government of India) for providing financial support for Cloud-Aerosol Interaction and Precipitation Enhancement Experiment (CAIPEEX). ASG is also thankful to the Department of Science and Technology, Government of India, for funding support under Climate Change Programme (CCP), SPLICE Division, Department of Science, New Delhi-110 016 (DST/CCP/Aerosol/83/2017(G).

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Correspondence to Alok Sagar Gautam or Sneha Gautam.

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Bisht, D.S., Srivastava, A.K., Singh, V. et al. High-Altitude Air Pollutants Monitored from Rainwater Chemistry in the Central Himalaya. Water Air Soil Pollut 233, 392 (2022). https://doi.org/10.1007/s11270-022-05855-8

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  • DOI: https://doi.org/10.1007/s11270-022-05855-8

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