scholarly journals Estimation of small-scale soil erosion in laboratory experiments with Structure from Motion photogrammetry

Geomorphology ◽  
2017 ◽  
Vol 295 ◽  
pp. 285-296 ◽  
Author(s):  
Matilde Balaguer-Puig ◽  
Ángel Marqués-Mateu ◽  
José Luis Lerma ◽  
Sara Ibáñez-Asensio
2014 ◽  
Vol 6 (8) ◽  
pp. 7050-7080 ◽  
Author(s):  
Andreas Kaiser ◽  
Fabian Neugirg ◽  
Gilles Rock ◽  
Christoph Müller ◽  
Florian Haas ◽  
...  

Since Franklin first showed that thunder and lightning are caused by electrical discharges, there have been numerous theories to account for the production of electricity in thunderstorms, but none has been generally accepted by meteorologists. When attacking the problems of thunderstorm electricity, two methods naturally present themselves: we may either investigate the actual phenomena in the atmosphere, or try to repeat on a small scale in the laboratory the processes which may be supposed to take place during thunderstorms. During 1907-8 an investigation was undertaken on both these lines at the Meteorological Office of the Government of India in Simla. A systematic record was obtained by automatic instruments of the electricity brought down by the rain during practically the whole of one rainy season, and laboratory experiments were made to find the origin of the electricity of thunderstorms. The work has resulted in the formation of a new theory, which appears to account in a satisfactory manner for the electrical effects observed during thunderstorms. The following paper is divided into three parts:—Part I deals with the measurements of the electricity of the rain, Part II with the laboratory experiments, and Part III contains the new theory based on the results detailed in the previous parts.


2013 ◽  
Vol 23 (6) ◽  
pp. 680-691 ◽  
Author(s):  
Shujie Zhang ◽  
Axing Zhu ◽  
Wenliang Liu ◽  
Jing Liu ◽  
Lin Yang

2018 ◽  
Vol 261 ◽  
pp. 136-143 ◽  
Author(s):  
Tongchuan Li ◽  
Ming’an Shao ◽  
Yuhua Jia ◽  
Xiaoxu Jia ◽  
Laiming Huang

Author(s):  
F. Carré ◽  
H.I. Reuter ◽  
J. Daroussin ◽  
O. Scheurer

2021 ◽  
Author(s):  
Ahsan Raza ◽  
Thomas Gaiser ◽  
Muhammad Habib-Ur-Rahman ◽  
Hella Ahrends

<p>Information on field scale soil erosion and related sedimentation process is very important for natural resource management and sustainable farming. Plenty of models are available for study of these processes but only a few are suitable for dynamic small scale soil erosion assessments. The available models vary greatly in terms of their input requirements, analysis capabilities, process [t1] complexities, spatial and temporal scale of their intended use, practicality, the manner they represent the processes, and the type of output information they provide. The study aims in examining, theoretically, 51 models classified as physical, conceptual, and empirical based on their representation of the processes of soil erosion. The literature review shows that there is no specific model available for soil erosion prediction under agroforestry systems.   It is further suggested that models like EPIC, PERFECT, GUEST, EPM, TCRP, SLEMSA, APSIM, RillGrow, and CREAMS can be potentially used for soil erosion assessment at plot/field scale at daily time steps. Most of these models are capable to simulate the soil erosion process at small scale; further model development is needed regarding their limitations with respect to components interaction i.e., rainfall intensity, overland flow, crop cover, and their difficulties in upscaling. The research suggested that SIMPLACE network can provide modules with LintulBiomass, HillFlow, Runoff to develop new dynamic components to simulate overland flow and soil erosion incorporating improved upscaling capabilities</p>


1997 ◽  
Vol 20 ◽  
pp. 9-26
Author(s):  
Antonio José Teixeira Guerra

The present paper concerns rill initiation and evolution, taking into account its role on the erosion process. Therefore, several aspects of the process are developed, such as: the process itself, evidences of the process, through field and laboratory experiments, the importance of the models, the consequences to agricultural soils and the conectivity with other soil erosion processes.


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