نتایج جستجو برای: a worldwide typical landform for aeolian erosion

تعداد نتایج: 16100361  

2008
Joel B. Sankey Matthew J. Germino

Wind erosion of soil is an appreciable but unstudied event following fires in cold desert. We examined aeolian transport of sediment for one year following fire in semiarid shrub steppe of southern Idaho. Sediment collectors were used to determine horizontal mass transport of soil ( ) and saltation sensors and anemometers were used to determine saltation activity (# seconds saltation is detecte...

2016
Lili Feng Zhiqing Jia Qingxue Li

Aeolian desertification is poorly understood despite its importance for indicating environment change. Here we exploit Gaofen-1(GF-1) and Moderate Resolution Imaging Spectroradiometer (MODIS) data to develop a quick and efficient method for large scale aeolian desertification dynamic monitoring in northern China. This method, which is based on Normalized Difference Desertification Index (NDDI) ...

2010
L. A. SPALLETTI

Permian red beds of the De La Cuesta Formation in the Sierra de Narváez (Paganzo Basin, northwestern Argentina) are essentially composed of sandstones associated with mudstones and subordinate conglomerates. Facies distributions and stacking patterns indicate that these sediments resulted from the interaction between aeolian and ephemeral fluvial systems, and are represented by aeolian dune, dr...

2017
Stephen Tooth

Definition Geomorphology is the science that studies the origin and development of landforms and how those landforms combine to form landscapes. Landforms are shaped by geomorphological processes, many of which involve the weathering, erosion, transportation, and deposition of surface materials (rock, sediment) by gravity, ice, wind, or water. Both erosional and depositional landforms can be id...

2018
Rebecca B. Abney Asmeret Asefaw Berhe

Pyrogenic carbon (PyC) constitutes an important pool of soil organic matter (SOM), particularly for its reactivity and because of its assumed long residence times in soil. In the past, research on the dynamics of PyC in the soil system has focused on quantifying stock and mean residence time (MRT) of PyC in soil, as well as determining both PyC stabilization mechanisms and loss pathways. Much o...

1996
RALPH D. LORENZ JONATHAN I. LUNINE

on which water ice has been positively identified. It is unlikely to be pure, although the nature, amount, and We examine various mechanisms of erosion on Titan and their likely effect on Titan’s geomorphology. Specifically we distribution of the contaminants (silicates, organics, and evaluate the solubility of likely crustal ices (water and ammoperhaps ammonia–water ice) are not known, but see...

Journal: :پژوهش های جغرافیای طبیعی 0
سیدمهدی پورباقر کردی مربی دانشگاه پیام نور و دانشجوی دکتری تخصصی ژئومورفولوژی، دانشگاه خوارزمی عزت الله قنواتی دانشیار گروه ژئومورفولوژی، دانشکدة علوم جغرافیا، دانشگاه خوارزمی امیر کرم دانشیار گروه ژئومورفولوژی، دانشکدة علوم جغرافیا، دانشگاه خوارزمی امیر صفاری دانشیار گروه ژئومورفولوژی، دانشکدة علوم جغرافیا، دانشگاه خوارزمی

introduction this research addresses the automatic extraction of alluvial fans using four methods of segmentation from satellite data. this segmentation method divides images into partitions. it is typically used to recognize objects or other relevant purposes in digital images (fu, 2013:3260). alluvial fans have always been a landform that attracts human because they are suitable areas for liv...

2003
D. M. GAIERO J.-L. PROBST P. J. DEPETRIS S. M. BIDART L. LELEYTER

The bulk of particulate transition metals transported by Patagonian rivers shows an upper crustal composition. Riverine particulate 0.5 N HCl leachable trace metal concentrations are mainly controlled by Fe-oxides. Complexation of Fe by dissolved organic carbon (DOC) appears to be an important determinant of the phases transporting trace metals in Patagonian rivers. In contrast, aeolian trace e...

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