Abstract
The paper presents the first data on the regional distribution of the isotopic composition of oxygen and hydrogen in waters, as well as the carbon of water-dissolved carbon dioxide in natural surface and underground infiltration waters of the Novosibirsk urban agglomeration. For the presented sample of samples, the vector of changes in the values of δD and δO in the studied region was obtained from -112 to -126 ‰ and from -14 to -16 ‰, respectively. The water-dissolved carbon dioxide of the studied waters has the expected biogenic genesis, the isotopic composition of carbon (δC from -14.0 to -7.0 ‰) indicates its participation in the processes of silicate-carbonate weathering.
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