机译:在青藏高原典型的热蚀沟中,紫外线而不是无机氮增加了溶解有机碳的生物降解能力
State Key Laboratory of Vegetation and Environmental Change, Institute of Botany, Chinese Academy of Sciences,University of Chinese Academy of Sciences;
State Key Laboratory of Vegetation and Environmental Change, Institute of Botany, Chinese Academy of Sciences;
State Key Laboratory of Vegetation and Environmental Change, Institute of Botany, Chinese Academy of Sciences;
State Key Laboratory of Vegetation and Environmental Change, Institute of Botany, Chinese Academy of Sciences,University of Chinese Academy of Sciences;
State Key Laboratory of Vegetation and Environmental Change, Institute of Botany, Chinese Academy of Sciences,University of Chinese Academy of Sciences;
State Key Laboratory of Vegetation and Environmental Change, Institute of Botany, Chinese Academy of Sciences,University of Chinese Academy of Sciences;
Alpine permafrost; Carbon cycle; Dissolved organic carbon; Thermokarst; Inorganic nitrogen; Ultraviolet radiation;
机译:泰国高原沟壑沟壑沟壑沟壑的散滤术轨迹
机译:解冻深度决定青藏高原北部溶解有机碳浓度和生物降解性
机译:溶解有机碳,溶解有机氮和溶解无机氮在热带湿林生态系统中的作用
机译:溶解无机氮和溶解无机磷测定仪的研制
机译:紫外线和可见辐射对安大略省中南部河流溶解的有机碳-铁相互作用的影响:颗粒状的碳和铁的形成,荧光光谱特征和铁的不稳定性。
机译:自动测定水样中总溶解无机碳和总不可溶解溶解有机碳的稳定碳同位素组成(013c / sup> C):RsIL实验室规范1851和1852