Isotopic ((13)C) fractionation during plant residue decomposition and its implications for soil organic matter studies.
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Comparing the effect of naturally restored forest and grassland on carbon sequestration and its vertical distribution in the Chinese Loess PlateauCarbon isotopic fractionation during decomposition of plant materials of different qualityIntegrating stand and soil properties to understand foliar nutrient dynamics during forest succession following slash-and-burn agriculture in the Bolivian Amazon.Carbon isotopes in terrestrial ecosystem pools and CO2 fluxes.An optical method for carbon dioxide isotopes and mole fractions in small gas samples: Tracing microbial respiration from soil, litter, and lignin.Precipitation pulse size effects on Sonoran Desert soil microbial crusts.Response of a soil bacterial community to grassland succession as monitored by 16S rRNA levels of the predominant ribotypesDifferential C isotope discrimination by fungi during decomposition of C(3)- and C(4)-derived sucrose.13C isotopic fractionation during biodegradation of agricultural wastes.Reliability of stable carbon and oxygen isotope compositions of pedogenic needle fibre calcite as environmental indicators: examples from Western Europe.Intraspecific carbon and nitrogen isotopic variability in foxtail millet (Setaria italica).Early-stage changes in natural (13)C and (15)N abundance and nutrient dynamics during different litter decomposition.Nitrogen isotopes suggest a change in nitrogen dynamics between the Late Pleistocene and modern time in Yukon, Canada.Rapid turnover of DOC in temperate forests accounts for increased CO2 production at elevated temperatures.Discrete taxa of saprotrophic fungi respire different ages of carbon from Antarctic soils.Soil Carbon Dynamics in Soybean Cropland and Forests in Mato Grosso, Brazil.Role of aggregate surface and core fraction in the sequestration of carbon from dung in a temperate grassland soilIsotopic discrimination during litter decomposition and delta13C and delta15N soil profiles in a young artificial stand and in an old floodplain forestThe application and interpretation of Keeling plots in terrestrial carbon cycle researchChemostratigraphic implications of spatial variation in the Paleocene-Eocene Thermal Maximum carbon isotope excursion, SE Bighorn Basin, WyomingLigno-aliphatic complexes in soils revealed by an isolation procedure: implication for lignin fate
P2860
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P2860
Isotopic ((13)C) fractionation during plant residue decomposition and its implications for soil organic matter studies.
description
1999 nî lūn-bûn
@nan
1999年の論文
@ja
1999年学术文章
@wuu
1999年学术文章
@zh-cn
1999年学术文章
@zh-hans
1999年学术文章
@zh-my
1999年学术文章
@zh-sg
1999年學術文章
@yue
1999年學術文章
@zh
1999年學術文章
@zh-hant
name
Isotopic ((13)C) fractionation ...... r soil organic matter studies.
@en
type
label
Isotopic ((13)C) fractionation ...... r soil organic matter studies.
@en
prefLabel
Isotopic ((13)C) fractionation ...... r soil organic matter studies.
@en
P2093
P1476
Isotopic ((13)C) fractionation ...... r soil organic matter studies.
@en
P2093
P304
P356
10.1002/(SICI)1097-0231(19990715)13:13<1284::AID-RCM578>3.0.CO;2-0
P577
1999-07-01T00:00:00Z