000 02786nlm1a2200445 4500
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.]
203 _aText
_celectronic
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-
463 _tVol. 52, iss. 1
_v[P. 36–43]
_d2018
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