標(biāo)題: Titlebook: Geomorphology of Desert Environments; Athol D. Abrahams,Anthony J. Parsons Book 19941st edition Athol D. Abrahams and Anthony J. Parsons 1 [打印本頁(yè)] 作者: ED431 時(shí)間: 2025-3-21 16:51
書(shū)目名稱Geomorphology of Desert Environments影響因子(影響力)
書(shū)目名稱Geomorphology of Desert Environments影響因子(影響力)學(xué)科排名
書(shū)目名稱Geomorphology of Desert Environments網(wǎng)絡(luò)公開(kāi)度
書(shū)目名稱Geomorphology of Desert Environments網(wǎng)絡(luò)公開(kāi)度學(xué)科排名
書(shū)目名稱Geomorphology of Desert Environments被引頻次
書(shū)目名稱Geomorphology of Desert Environments被引頻次學(xué)科排名
書(shū)目名稱Geomorphology of Desert Environments年度引用
書(shū)目名稱Geomorphology of Desert Environments年度引用學(xué)科排名
書(shū)目名稱Geomorphology of Desert Environments讀者反饋
書(shū)目名稱Geomorphology of Desert Environments讀者反饋學(xué)科排名
作者: Entrancing 時(shí)間: 2025-3-21 21:20
Masanori Uchikawa,Tatsuya Takemototical in determining the threshold of operation of runoff, through its impact on infiltration. Since infiltration is one of the major thresholds in dryland morphological development, the factors which control it have a role out of all proportion to the energy involved.作者: Agnosia 時(shí)間: 2025-3-22 03:33 作者: 典型 時(shí)間: 2025-3-22 07:56 作者: 受傷 時(shí)間: 2025-3-22 09:53 作者: PET-scan 時(shí)間: 2025-3-22 16:28
électronique et optoélectronique organiquestrongly influenced by the physical and chemical characteristics of the underlying soils. As a result, the evolution of a diversity of desert landforms is either directly or indirectly linked to pedogenic processes.作者: PET-scan 時(shí)間: 2025-3-22 18:20 作者: Pcos971 時(shí)間: 2025-3-22 21:41 作者: Spartan 時(shí)間: 2025-3-23 04:24 作者: Sleep-Paralysis 時(shí)間: 2025-3-23 07:46
Electroslag Remelting Towards Clean Steel Gran Sabana of south-east Venezuela, a broadly upwarped region of gently dipping early Proterozoic strata, pediments comprise the floors of broad subsequent valleys developed within less resistant parts of the section (Dohrenwend .. 1994b).作者: attenuate 時(shí)間: 2025-3-23 10:23
Rock-Mantled Slopes. These processes are not only important in terms of understanding hillslope form but because they give rise to a variety of hydrologic and geomorphic phenomena such as flash flooding, extreme soil erosion, and hazardous debris flows.作者: Arthropathy 時(shí)間: 2025-3-23 17:09
Channel Processes, Evolution, and Historyal basis of the subject at the end of the 20th century still bears a heavy imprint from the American source. In the Old World, only the Israelis, under A. Schick, have been able to maintain such a strong contribution to desert fluvial geomorphology.作者: 蒸發(fā) 時(shí)間: 2025-3-23 22:07
Pediments in Arid Environments Gran Sabana of south-east Venezuela, a broadly upwarped region of gently dipping early Proterozoic strata, pediments comprise the floors of broad subsequent valleys developed within less resistant parts of the section (Dohrenwend .. 1994b).作者: 行業(yè) 時(shí)間: 2025-3-23 22:10
Geomorphology of Desert Environmentstable measure of aridity upon which to base a definition of desert areas has not been straightforward, and several attempts based upon a variety of geomorphic, climatic, and/or vegetational indices of aridity have been made to identify the world distribution of deserts.作者: 能得到 時(shí)間: 2025-3-24 05:01
Aridic Soils, Patterned Ground, and Desert Pavementstrongly influenced by the physical and chemical characteristics of the underlying soils. As a result, the evolution of a diversity of desert landforms is either directly or indirectly linked to pedogenic processes.作者: 同步左右 時(shí)間: 2025-3-24 09:04 作者: 下垂 時(shí)間: 2025-3-24 13:02
Chapitre 7 Librairies de SimPowerSystems,lectures or paper presentations. This chapter will therefore concentrate upon some of the less certain issues in weathering studies. The aim is not to be exhaustive or comprehensive, but hopefully to question some traditionally held views and stimulate future research.作者: Cantankerous 時(shí)間: 2025-3-24 15:06 作者: Progesterone 時(shí)間: 2025-3-24 22:56 作者: ovation 時(shí)間: 2025-3-25 01:37 作者: FECK 時(shí)間: 2025-3-25 04:53
Weathering Processes and Formslectures or paper presentations. This chapter will therefore concentrate upon some of the less certain issues in weathering studies. The aim is not to be exhaustive or comprehensive, but hopefully to question some traditionally held views and stimulate future research.作者: GROUP 時(shí)間: 2025-3-25 09:11
Rock Varnish in Deserts In seasonally flooded tropical riverine environments, vitreous silica-rich films of brown to purple-black colour are sometimes present on exposed bedrock potholes (Tricart 1972) and point bar cobbles, which may be cemented together to form a resistant carapace.作者: Collected 時(shí)間: 2025-3-25 15:39
Badlandsect of direct observational coupling of process and landform evolution in both natural and man-induced badlands. However, Campbell (1989) and Campbell and Honsaker (1982) caution about problems of scaling between processes on badland slopes and channels to larger landforms.作者: collateral 時(shí)間: 2025-3-25 18:01 作者: 你正派 時(shí)間: 2025-3-25 23:18 作者: dissent 時(shí)間: 2025-3-26 04:07 作者: offense 時(shí)間: 2025-3-26 07:43 作者: tenuous 時(shí)間: 2025-3-26 10:55 作者: cartilage 時(shí)間: 2025-3-26 14:57 作者: neurologist 時(shí)間: 2025-3-26 19:49
https://doi.org/10.1007/978-3-642-61962-5mboldt (1819). These surface films are most conspicuous in arid regions (e.g. Laudermilk 1931), where exposed rock outcrops and rubble deposits are ubiquitous and frequently are covered by glossy, brown to black, iron- and/or manganese-rich patinas, giving rise to the term desert varnish. Beyond the作者: 調(diào)色板 時(shí)間: 2025-3-27 00:50
https://doi.org/10.1007/978-3-642-79069-0parseness of vegetation, results in more widespread occurrence of slopes with little or no regolith than in areas with humid climates. This chapter outlines the processes and landforms occurring on desert slopes that are either massive bedrock or are scarps and cuestas in layered rocks dominated by 作者: Nonthreatening 時(shí)間: 2025-3-27 03:02
https://doi.org/10.1007/978-3-319-30012-2hich are dealt with in Chapters 13 and 14) nor are developed in highly erodible, fine-grained sedimentary rocks (i.e. badlands slopes, which are treated in Chapter 9). Such hillslopes in desert (arid and semi-arid) climates are usually mantled with a thin layer of coarse debris that has either weath作者: coalition 時(shí)間: 2025-3-27 05:24 作者: harangue 時(shí)間: 2025-3-27 12:05
https://doi.org/10.1007/978-1-4684-1755-5 are fluvial and aeolian, which operate on a surface with a very reduced vegetation cover. Indeed vegetation is absent in many areas. Even in more favourable locations plant cover may not reach 50%, giving an impression of the predominance of bare ground. Biogenic processes affecting landform evolut作者: maintenance 時(shí)間: 2025-3-27 16:28
Masanori Uchikawa,Tatsuya Takemotothat exist; secondly, as a chemical substance which interacts with other chemical substances, notably salts; third, as a medium of transport of mass; and, fourth, as a direct source of energy. The last role, though small by comparison with the roles of solar and wind energy, may none the less be cri作者: 祖?zhèn)髫?cái)產(chǎn) 時(shí)間: 2025-3-27 21:11
Petra Sim?i?,Alessio Pierini,George Lubas-arid areas. This is due largely to the originality, forcefulness, and intellectual background of American geomorphologists developed during and sustained long after the exploration of the American West. The strong sense of field observation and experiment coupled with a deep historical perspective,作者: Concrete 時(shí)間: 2025-3-28 01:09
Electroslag Remelting Towards Clean Steelings. Reported on six continents, their distribution spans the range of subpolar latitudes from the Arctic to the Antarctic and the range of climate from hyperarid to humid tropical (Whitaker 1979). On the Cape York Peninsula in tropical north-east Queensland, a tecto-nically quiescent region of Pre作者: 使成波狀 時(shí)間: 2025-3-28 05:23 作者: Expurgate 時(shí)間: 2025-3-28 06:57 作者: HAUNT 時(shí)間: 2025-3-28 12:37
Overview: Over the last twenty years there has been a major expansion ofknowledge in the field of landforms and landforming processes ofdeserts. This advanced-level book provides a benchmark for thecurrent state of science, and is written by an international team ofauthors who are acknowledged experts in their fields.978-94-015-8254-4作者: Palter 時(shí)間: 2025-3-28 18:32 作者: 猛擊 時(shí)間: 2025-3-28 20:36 作者: Graphite 時(shí)間: 2025-3-28 23:04
Duricrustsete, silcrete, and gypcrete. Collectively, these are referred to as duricrusts (Woolnough 1930). This chapter focuses on the morphology, chemistry, mineralogy, and origin of the major types of crusts. Particular attention is given to recent research from Australia, the United States, and Africa.作者: senile-dementia 時(shí)間: 2025-3-29 04:40 作者: 迷住 時(shí)間: 2025-3-29 07:54 作者: LATHE 時(shí)間: 2025-3-29 13:54
https://doi.org/10.1007/978-94-015-8254-4erosion; geomorphology; hydrology; transport; hydrogeology作者: BROTH 時(shí)間: 2025-3-29 17:14
Geomorphology of Desert Environmentse, however, areas of aridity, and it is upon this property that the scientific definition of deserts has generally hinged. Even so, providing an acceptable measure of aridity upon which to base a definition of desert areas has not been straightforward, and several attempts based upon a variety of ge作者: 合適 時(shí)間: 2025-3-29 21:16 作者: 具體 時(shí)間: 2025-3-30 02:39
Weathering Processes and Formslandforms with which they are generally associated. Invariably such reviews — especially if orientated towards students — deal primarily with the perceived certainties of our knowledge. In reality, however, weathering studies are more characterized by uncertainties and gaps in knowledge. Weathering 作者: SUE 時(shí)間: 2025-3-30 06:27 作者: 大炮 時(shí)間: 2025-3-30 08:20
Duricrustsete, silcrete, and gypcrete. Collectively, these are referred to as duricrusts (Woolnough 1930). This chapter focuses on the morphology, chemistry, mineralogy, and origin of the major types of crusts. Particular attention is given to recent research from Australia, the United States, and Africa.作者: Euphonious 時(shí)間: 2025-3-30 13:25
Rock Varnish in Desertsmboldt (1819). These surface films are most conspicuous in arid regions (e.g. Laudermilk 1931), where exposed rock outcrops and rubble deposits are ubiquitous and frequently are covered by glossy, brown to black, iron- and/or manganese-rich patinas, giving rise to the term desert varnish. Beyond the作者: enumaerate 時(shí)間: 2025-3-30 19:41 作者: Slit-Lamp 時(shí)間: 2025-3-30 21:03
Rock-Mantled Slopeshich are dealt with in Chapters 13 and 14) nor are developed in highly erodible, fine-grained sedimentary rocks (i.e. badlands slopes, which are treated in Chapter 9). Such hillslopes in desert (arid and semi-arid) climates are usually mantled with a thin layer of coarse debris that has either weath作者: GUILE 時(shí)間: 2025-3-31 03:21
Badlandssity, shallow to non-existent regolith, and rapid erosion rates. Badlands appear to offer in a miniature spatial scale and a shortened temporal scale many of the processes and landforms exhibited by more normal fluvial landscapes, including a variety of slope forms, bedrock or alluvium-floored rills作者: upstart 時(shí)間: 2025-3-31 07:41
Plants on Desert Hillslopes are fluvial and aeolian, which operate on a surface with a very reduced vegetation cover. Indeed vegetation is absent in many areas. Even in more favourable locations plant cover may not reach 50%, giving an impression of the predominance of bare ground. Biogenic processes affecting landform evolut作者: 表示向前 時(shí)間: 2025-3-31 13:05
Catchment and Channel Hydrologythat exist; secondly, as a chemical substance which interacts with other chemical substances, notably salts; third, as a medium of transport of mass; and, fourth, as a direct source of energy. The last role, though small by comparison with the roles of solar and wind energy, may none the less be cri作者: miscreant 時(shí)間: 2025-3-31 13:49
