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Effects of peat decomposition on δ 13 C and δ 15 N depth profiles of Alpine bogs of stable carbon and nitrogen isotopes (δ 13 C and δ 15 N) in soils and peats. However, the applicability
Effects of peat decomposition on δ 13 C and δ 15 N depth profiles of Alpine bogs for the signatures of stable carbon and nitrogen isotopes (δ 13 C and δ 15 N) in soils and peats. However
Effects of peat decomposition on δ 13 C and δ 15 N depth profiles of Alpine bogsEffects of peat decomposition on δ 13 C and δ 15 N depth profiles of Alpine
Способ обнаружения отказов при экономичном резервировании бортового оборудования беспилотного летательного аппарата
Land use change decreases soil carbon stocks in Tibetan grasslands to cropland. Detailed SOC measurements up to 30-cm depth were combined with analysis of δ13C, δ15N, bulk
Land use change decreases soil carbon stocks in Tibetan grasslands to cropland. Detailed SOC measurements up to 30-cm depth were combined with analysis of δ13C, δ15N, bulk
Единственность классического решения основной начально-краевой задачи для квазигидродинамических уравнений
Soil organic matter turnover: Global implications from δ13C and δ15N signatures gases fluxes. Based on the global database of the stable isotope composition of C (δ13C) and N (δ15N
Δ2 0 -copies of linear orderingsIt is proved that, for any n ω, there exist countable linear orderings Ln whose Δ 2 0 -spectrum
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