机译:人为强迫对表面O周期的影响
Water Environment Technology, Department of Civil and Environmental Engineering, Chalmers University of Technology, 41296 Goeteborg, Sweden;
Department of Marine Chemistry and Geochemistry, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts 02543;
Department of Geology and Geochemistry, Stockholm University, 10691 Stockholm, Sweden;
Earth Science and Engineering, Imperial College London, SW72AZ London, U.K., Mineralogy, The Natural History Museum, London, SW7 5PD, London U.K.;
Edafologia y Quimica Agricola, Facultad de Biologia, Universidad de Santiago de Compostela-Catnpus Sur, 15782 Santiago, Spain;
Department of Geosciences, University of Bremen, 28359 Bremen, Germany;
Departament de FisicaUniversitat Autbnoma de Barcelona, E-08193 Bellaterra, Spain;
School of Geosciences, University of Aberdeen, Aberdeen, AB243UF, Scotland, U.K.;
epartment of Civil and Environmental Engineering, Massachusetts institute of Technology, Cambridge, Massachusetts 02139;
机译:地中海东部磷和氮循环的生物地球化学模型,第2部分。营养循环和初级生产对人为强迫的响应:1950-2000年
机译:渗透性浅层含水层的盐分影响边界处的氧化还原带:物理强迫对铁和锰的生物地球化学循环的影响
机译:降水周期的破坏:人为强迫的归因
机译:快速绘制海洋表层沉积物中人为放射性核素,金属和有机化合物的图
机译:人为干扰对河岸湿地土壤铁和氮循环的影响。
机译:表层水生沉积物中氮和硫循环的环境控制
机译:降水循环中断:对人为迫使的归因