کد مقاله کد نشریه سال انتشار مقاله انگلیسی نسخه تمام متن
5161395 1502253 2017 46 صفحه PDF دانلود رایگان
عنوان انگلیسی مقاله ISI
Thermally altered marine dissolved organic matter in hydrothermal fluids
ترجمه فارسی عنوان
مواد معدنی محلول در آب به صورت حرارتی در مایعات هیدروترمال تجزیه می شوند
کلمات کلیدی
سیستم هیدروترمال، ماده آلی حل شده، تجزیه حرارتی، ماده آلی مقاوم در برابر، طیف سنجی جرمی سیکلوترون یون تبدیل تبدیل فوریه،
موضوعات مرتبط
مهندسی و علوم پایه شیمی شیمی آلی
چکیده انگلیسی
Hydrothermal vent fluids contain thermally modified dissolved organic matter (DOM) originally entrained from sediments and seawater. We hypothesized that in hydrothermal systems DOM molecular composition is modulated by (i) fluid contribution, (ii) thermal decomposition and pH, and (iii) aspects particular to the vent system. Hence, solid phase extracted (SPE) DOM samples collected along the Mid-Atlantic Ridge (MAR) were molecularly characterized via 15 Tesla Fourier transform ion cyclotron resonance mass spectrometry (FT-ICR-MS). The molecular character of an oceanic DOM sample was also determined before and after thermal (300 °C) decomposition at acidic and neutral pH. Multivariate statistical analysis indicated that DOM composition was strongly influenced by fluid contribution (Mg2+ concentration between 12 and 54 mM), which correlated positively with measured temperature (between 8 and 375 °C). In comparison, pH of the fluids (between 2.5 and 6.9) had a minor influence. Seafloor pressure, used as a theoretical maximum fluid temperature at the seafloor, separated the fluids collected at Menez Gwen from deeper locations, due to the higher abundance of peptide, carboxyl-rich alicyclic (CRAM) and aromatic molecular formulae at Menez Gwen. Compared with seawater DOM, thermally decomposed DOM had on average lower molecular mass, lower O/C ratios, fewer double bond equivalents, and fewer CRAM formulae but higher aromaticity - the same molecular features displayed by MAR hydrothermal fluids. The study provides evidence that thermal reworking plays a major role in shaping DOM mixtures from hydrothermal fluids along the MAR, which partly represent thermally reworked marine DOM that survived hydrothermal circulation.
ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Organic Geochemistry - Volume 110, August 2017, Pages 73-86
نویسندگان
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