Tools in Fluvial Geomorphology 2016
DOI: 10.1002/9781118648551.ch2
|View full text |Cite
|
Sign up to set email alerts
|

Surficial geological tools in fluvial geomorphology

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
3
1
1

Citation Types

0
3
0
2

Year Published

2017
2017
2022
2022

Publication Types

Select...
5
1
1

Relationship

0
7

Authors

Journals

citations
Cited by 10 publications
(5 citation statements)
references
References 123 publications
0
3
0
2
Order By: Relevance
“…To close the concept, we define the flood stage as an established gauge height for a given location above which a rise in water surface level begins to create a hazard [5]. We identified it with the bankfull stage from the proto-floodplain (top of the point bar surface) that supports woody vegetation [49].…”
Section: Effects Of Vegetation Encroachment and Aggradation On Channementioning
confidence: 99%
See 1 more Smart Citation
“…To close the concept, we define the flood stage as an established gauge height for a given location above which a rise in water surface level begins to create a hazard [5]. We identified it with the bankfull stage from the proto-floodplain (top of the point bar surface) that supports woody vegetation [49].…”
Section: Effects Of Vegetation Encroachment and Aggradation On Channementioning
confidence: 99%
“…Table A1 summarises the characteristic dimensions of the meanders in Figure 1. To evaluate them, we determined the bankfull stage from the proto-floodplain (top of the point bar surface) that supports woody vegetation, as suggested in [49]. Table A1.…”
Section: Conflicts Of Interestmentioning
confidence: 99%
“…Chronosequence frameworks have improved understanding of the rates and pathways of primary mineral weathering [4,5], clay mineral transformations [6,7], and changes to bulk chemistry [8,9] in soils from a range of global settings. Furthermore, when the time required to develop certain pedogenic features is known, soil chemical and mineralogical properties are useful for establishing relative-age relationships among landforms [5,10], mapping and correlating Quaternary deposits [11], and aiding chronological interpretations in archaeological investigations [12,13]. Given these attributes, soil chronosequences serve important functions in pedology, geomorphology, archaeology, and Quaternary geology [3].…”
Section: Introductionmentioning
confidence: 99%
“…Apesar de ser comumente tratada como subárea da Geografi a, ela demanda (e ao mesmo tempo fornece) conhecimentos da Geologia, Biologia e engenharias, entre outras ciências, o que revela sua diversidade e amplitude. Questões relativas à dinâmica fl uvial podem envolver uma grande variedade de escalas temporais -segundos a eras geológicas -e espaciais -de manchas individuais de habitats à evolução de bacias de drenagem de escala continental (Jacobson et al, 2003).…”
Section: Introductionunclassified
“…Assim, a interpretação do passado e da história geomorfológica (em termos evolutivos) dos cursos d'água e da rede de drenagem seria embasada pelas evidências atuais, principalmente as características dos registros sedimentares. Por outro lado, uma compreensão do passado pode ser a chave para se entender o futuro, no sentido de que a história de um sistema fl uvial pode fornecer subsídios para a compreensão das características naturais de um curso d'água e, dessa forma, servir como referencial para avaliações, restaurações e previsões (Jacobson et al, 2003), trazendo inúmeros benefícios e possibilidades para o planejamento territorial e manejo de sistemas hídricos.…”
Section: Introductionunclassified