scispace - formally typeset
D

Daria M. Kuzmina

Researcher at Tomsk State University

Publications -  9
Citations -  141

Daria M. Kuzmina is an academic researcher from Tomsk State University. The author has contributed to research in topics: Permafrost & Peat. The author has an hindex of 4, co-authored 4 publications receiving 71 citations.

Papers
More filters
Journal ArticleDOI

Dissolved organic carbon and major and trace elements in peat porewater of sporadic, discontinuous, and continuous permafrost zones of western Siberia

TL;DR: In this article, the authors collected soil porewaters from 30 cm depth using suction cups and analyzed dissolved organic carbon (DOC), dissolved inorganic carbon (DIC), and 40 major elements and TEs in 0.45 µm filtered fraction of 80 porewater solutions.
Journal ArticleDOI

Dispersed ground ice of permafrost peatlands: Potential unaccounted carbon, nutrient and metal sources.

TL;DR: It is proposed a global peat ice inventory in permafrost regions is essential for assessing the consequences ofpermafrost thaw on surface aquatic systems.
Journal ArticleDOI

Colloidal organic carbon and trace elements in peat porewaters across a permafrost gradient in Western Siberia

TL;DR: In this paper, the authors studied colloids in peat porewaters across a natural gradient of sporadic, isolated, discontinuous and continuous permafrost zone in the Western Siberian Lowland (WSL), the largest peatland in the world.
Journal ArticleDOI

Microtopography Controls of Carbon and Related Elements Distribution in the West Siberian Frozen Bogs

TL;DR: In this paper, the authors investigated how the microtopographic features of the landscape affect the thermal and hydrologic conditions of the soil as well as the nutrient availability and consequently, the dynamics of carbon and related elements.
Journal ArticleDOI

Organic carbon, and major and trace elements reside in labile low-molecular form in the ground ice of permafrost peatlands: a case study of colloids in peat ice of Western Siberia.

TL;DR: In this paper , the authors used a size fractionation procedure (centrifugal ultrafiltration) to quantify the proportion of colloidal (3 kDa to 0.45 μm) and conventionally dissolved low molecular weight (LMW < 3 kDa) fractions of DOC, and major and trace elements in the porewater and ice of 5 peat cores sampled along a 400 km permafrost and climate gradient in the largest peatland in the world, the Western Siberian Lowland.