000 | 02786nlm1a2200445 4500 | ||
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001 | 658165 | ||
005 | 20231030041541.0 | ||
035 | _a(RuTPU)RU\TPU\network\25372 | ||
035 | _aRU\TPU\network\23995 | ||
090 | _a658165 | ||
100 | _a20180618a2018 k y0engy50 ba | ||
101 | 0 | _aeng | |
102 | _aUS | ||
135 | _adrcn ---uucaa | ||
181 | 0 | _ai | |
182 | 0 | _ab | |
200 | 1 |
_aConcentrations and Composition of Sphagnum Peat Lipids Depending on Temperature in the Climatic Zones of Western Siberia _fO. V. Serebrennikova [et al.] |
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203 |
_aText _celectronic |
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300 | _aTitle screen | ||
320 | _a[References: p. 43 (15 tit.)] | ||
330 | _aThe composition of n-alkanes; sesqui-, di-, and triterpenoids; steroids; carboxylic acids; and tocopherols of sphagnum peat from the southern, middle, and northern taiga and forest-tundra of Western Siberia was studied by gas chromatography–mass spectrometry. It was shown that the latitudinal shift to the north leads to the preservation of the peat lipid components and sufficiently high values of carbon preference index (CPI) close to those of mire plants. This can be caused by a decrease in microbiological activity due to a decrease in the mean annual temperature. Towards the north, the total concentrations of n-alkanes, steroids, pentacyclic triterpenoids, squalene, and tocopherols increased, and a ratio of the total concentration of steroids to the concentrations of pentacyclic triterpenoids and hopanes decreased. | ||
333 | _aРежим доступа: по договору с организацией-держателем ресурса | ||
461 |
_tSolid Fuel Chemistry _d1974- |
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463 |
_tVol. 52, iss. 1 _v[P. 36–43] _d2018 |
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610 | 1 | _aэлектронный ресурс | |
610 | 1 | _aтруды учёных ТПУ | |
610 | 1 | _aторфяные ресурсы | |
610 | 1 | _aЗападная Сибирь | |
610 | 1 | _aклиматические зоны | |
610 | 1 | _aлипиды | |
610 | 1 | _aсфагновый торф | |
610 | 1 | _aхромато-масс-спектрометрия | |
701 | 1 |
_aSerebrennikova _bO. V. _cgeochemist _cProfessor of Tomsk Polytechnic University, Doctor of chemical sciences _f1949- _gOlga Viktorovna _2stltpush _3(RuTPU)RU\TPU\pers\30954 |
|
701 | 1 |
_aDuchko _bM. A. _gMariya Aleksandrovna |
|
701 | 1 |
_aKoronatova _bN. G. |
|
701 | 1 |
_aStrelnikova _bE. B. |
|
712 | 0 | 2 |
_aНациональный исследовательский Томский политехнический университет _bИнженерная школа природных ресурсов _bОтделение геологии _h8083 _2stltpush _3(RuTPU)RU\TPU\col\23542 |
801 | 2 |
_aRU _b63413507 _c20180618 _gRCR |
|
856 | 4 | _uhttps://doi.org/10.3103/S0361521918010081 | |
942 | _cCF |