“砖红壤”的概念、定义、翻译、参考文献-科学参考

单词	砖红壤
释义	砖红壤 Encyclopedia 农学砖红壤释 Latosol砖红壤强酸性、高铁铝氧化物的暗红色土壤。通常在热带高温高湿、强度淋溶条件下由富铁铝化作用形成。砖红壤在中国土壤系统分类中（1998），列为湿热铁铝土亚纲、铁铝土土纲；在中国土壤系统分类（2001）中，归属在湿润铁铝土[注]、湿润富铁土[注]或湿润雏形土[注]；在美国土壤系统分类（1999）中，大致相当于湿润氧化土[注]、湿润老成土[注]或湿润始成土[注]；在世界土壤资源参比基础（2014）中，大致相当于铁铝土[注]、低活性强酸土[注]、雏形土[注]等。
随便看	School of Design, The HongKong Polytechnic University School of Design, University of Edinburgh School of Design，Hunan University School of Design，Jiangnan University School of drama, film and television, Shandong Academy of Arts school of experimental pedagogy School of Film and Media Studies, Singapore Ngee Ann Polytechnic School of Film and New Media，Taipei National University of the Arts school of historical sociology School of history and archives, Russian National University of Humanities School of History and Culture of Science,Shanghai Jiao Tong University school of human ecology School of Industrial Design， Nan Jing University of Art School of Infancy: An Essay on the Education of Youth During the First Six Years School of Information and Library Science, University of North Carolina at Chapel Hill School of Information Management, NanJing University School of Information Management, Wuhan University School of Information Resources Management in RenMin University of China School of Information Sciences, University of Pittsburgh School of Information Science,Sun Yat-Sen University School of Information Studies,Syracuse University School of Information,The University of Texas at Austin School of Information, University of Michigan school of integration of Traditional Chinese and Western Medicine School of Journalism and Communication Renmin University of China

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