თბილისში COVID-19-ის გავრცელებაზე მიწისპირა ოზონის კონცენტაციის გავლენის კვლევის შედეგები

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ა. ამირანაშვილი
ნ. ჯაფარიძე
ჯ. ხარჩილავა
კ. ხაზარაძე
ა. რევიშვილი

ანოტაცია

წარმოდგენილია მიწისქვეშა ოზონის კონცენტრაციის (SOC) დღიური მნიშვნელობების   ქალაქ თბილისის მოსახლეობის კორონავირუსით ინფიცირების დადებითობის მაჩვენებელზე COVID-19 (IR) კვლევის შედეგები 2020 წლის 8 ოქტომბრიდან  2021 წლის 31 მაისამდე. აღმოჩნდა, რომ IR მნიშვნელობები საპირისპირო კორელაციაშია SOC-თან. მაგალითად, ოზონის კონცენტრაციებისთვის 0-დან 20 მკგ/მ3-მდე, COVID-19  ინფექციის პოზიტიურობის მაჩვენებელი საშუალოდ შეადგენდა 18.5%-ს, ხოლო SOC-ის მნიშვნელობებისთვის 80-დან 100 მკგ/მ3-მდე იყო მხოლოდ 2.3%. ყოველდღიურ IR მნიშვნელობებსა და SOC-ის შორის ურთიერთობას აქვს შებრუნებული წრფივი ფორმა. IR = -0,2307·SOC + 20.543 ინდივიდუალური შემთხვევებისთვის; IR = -0,2113·SOC + 19.756 - საშუალო IR მნიშვნელობებისთვის SOC-ის მნიშვნელობების სხვადასხვა დიაპაზონში.

საკვანძო სიტყვები:
მიწისპირა ოზონის კონცენტრაცია, СOVID-19, დადებითობის მაჩვენებელი.
გამოქვეყნებული: Dec 28, 2023

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ამირანაშვილი ა., ჯაფარიძე ნ., ხარჩილავა ჯ., ხაზარაძე კ., & რევიშვილი ა. (2023). თბილისში COVID-19-ის გავრცელებაზე მიწისპირა ოზონის კონცენტაციის გავლენის კვლევის შედეგები. საქართველოს გეოფიზიკური საზოგადოების ჟურნალი, 26(2). https://doi.org/10.60131/ggs.2.2023.7446
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