Ecological and geochemical studies of clastic material from the Bureya landslide after cyclic freezing/thawing in vitro

Мұқаба

Дәйексөз келтіру

Толық мәтін

Ашық рұқсат Ашық рұқсат
Рұқсат жабық Рұқсат берілді
Рұқсат жабық Тек жазылушылар үшін

Аннотация

The paper presents the results of experimental study (in vitro) of the transformation of clastic material (CM) sampled from a landslide body at the Bureya water reservoir. СM samples are considered as a model for assessing the influence of abiogenic and biogenic factors on the transformation (destruction, dissolution) of Si-containing minerals under various conditions of cyclic freezing/thawing, i. e., the dry sample; the samples placed in deionized water and in the presence of a solution of low molecular weight peptides. Freezing was carried out at a temperature of –18 °C, and thawing at a different temperature range (+4°C and +23°C). The elemental composition of aqueous solutions was determined by ICP-MS, and the microstructure of the CM surface was determined using scanning electron microscopy. As a result of 5 cycles after 7 days of freezing/thawing of CM samples in deionized water, the content of water-soluble forms of chemical elements (Fe, Ni, Cu, Zn, As, Mo, Ag, Cd, Tl, Bi, As) was below the detection limits of the device (< 0.001 µg/l). However, in the presence of a nutrient medium with peptone and a natural microbial consortium that retained its viability, the concentrations of a number of elements (Al, Ca, Mg, Fe, Mn, As, Hg) in the aquatic environment increased significantly. According to SEM images, a significant change in the microstructure of the surface of the samples CM occurred regardless of the thawing temperature when microorganisms were activated by low-molecular peptides. The formation of biofilms on the surface of CM grains was accompanied by the formation of various isomorphic microaggregates.

Толық мәтін

Рұқсат жабық

Авторлар туралы

L. Kondratyeva

Institute of Water and Ecology Problems, Far Eastern Branch, Russian Academy of Sciences

Хат алмасуға жауапты Автор.
Email: kondratevalm@gmail.com
Ресей, ul. Dikopol’tseva 56, Khabarovsk, 680000

E. Golubeva

Institute of Tectonics and Geophysics, Far Eastern Branch, Russian Academy of Sciences; Pacific National University

Email: evg8302@yandex.ru
Ресей, ul. Kim Yu Chen 65, Khabarovsk, 680000; ul. Tiкhookeanskaya 136, Khabarovsk, 680035

N. Konovalova

Institute of Tectonics and Geophysics, Far Eastern Branch, Russian Academy of Sciences

Email: turtle_83@rambler.ru
Ресей, ul. Kim Yu Chen 65, Khabarovsk, 680000

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2. Fig. 1. General characteristics of the elemental composition of the OM samples used in the experiment.

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3. Fig. 2. Proof of the viability of microorganisms after 30 days of freezing at –18°C of OM samples: a – dry sample; b – sample in H2O/D; c – sample in the presence of peptone.

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4. Fig. 3. SEM images of the surface of the OM sample in deionized water at defrosting temperature: a, b – 4°C (×2000; ×10000); c, d – 23°C (×1000; ×10000).

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5. Fig. 4. SEM image and elemental composition of individual loci of the OM particle surface in an aqueous solution with peptone after cyclic freezing (–18°C) and thawing at a temperature of: a – 4°C (spectra 229–231); b – 23°C (spectra 232–236). MB – bacterial microcolonies, SF – spheroids; KA – colloidal agglomerates; SM – scaly microstructure; SP – stack of plates.

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