机译:生物黄土结皮在半干旱环境下形成黄土的重要性
Laboratory for Paleoemironmental Reconstruction, Faculty of Sciences, University of Novi Sad, Trg D. Obradovica 2, 21000 Novi Sad, Serbia;
Laboratory for Paleoemironmental Reconstruction, Faculty of Sciences, University of Novi Sad, Trg D. Obradovica 2, 21000 Novi Sad, Serbia;
Laboratory for Paleoemironmental Reconstruction, Faculty of Sciences, University of Novi Sad, Trg D. Obradovica 2, 21000 Novi Sad, Serbia,Centre for Quaternary Research, Department of Geography, Royal Holloway, University of London, Egham, Surrey TW20 0EX, UK;
Biological and Environmental Sciences, School of Natural Sciences, University of Stirling, Stirling FK9 4LA, UK;
Giotto Loess Research Group, Department of Geology, Leicester University, LE1 7RH, UK;
Laboratory for Paleoemironmental Reconstruction, Faculty of Sciences, University of Novi Sad, Trg D. Obradovica 2, 21000 Novi Sad, Serbia;
Laboratory for Paleoemironmental Reconstruction, Faculty of Sciences, University of Novi Sad, Trg D. Obradovica 2, 21000 Novi Sad, Serbia;
Laboratory for Paleoemironmental Reconstruction, Faculty of Sciences, University of Novi Sad, Trg D. Obradovica 2, 21000 Novi Sad, Serbia;
Laboratory for Paleoemironmental Reconstruction, Faculty of Sciences, University of Novi Sad, Trg D. Obradovica 2, 21000 Novi Sad, Serbia;
Geomorphology, University of Bayreuth, 95440 Bayreuth, Germany;
机译:半干旱黄土高原地区利用集水系统微植结皮造林的初步结果
机译:黄土高原半干旱区微集水集水系统绿化结皮造林的初步结果。
机译:青藏高原东北部山区黄土和黄土类沉积物的时空分布。 (特刊:黄土和尘埃动力学,环境,地形和成岩作用:向爱德华·德比郡致敬。)
机译:生物土壳的人工培养及其对中国黄土高原模拟降雨下的径流和渗透的影响
机译:明尼苏达州东南部的第四纪晚期景观演化:黄土,风沙和周缘环境。
机译:黄土环境下地表水文学对生物结皮微观形态的响应
机译:基于典范对应分析的黄土高原坡地生物土壤结壳的空间分布