On the relationship between suspended sediment concentration, rainfall variability and groundwater: an empirical and probabilistic analysis for the Andean Beni River, Bolivia (2003–2016)

Autor: Jhan Carlo Espinoza, José Max Ayala, Jorge Molina-Carpio, Elisa Natalia Armijos Cardenas, Naziano Filizola, Raúl Espinoza-Villar, Omar Gutierrez-Cori, Ana Claudia Callau Poduje, Irma Ayes Rivera
Jazyk: angličtina
Rok vydání: 2019
Předmět:
Dewey Decimal Classification::500 | Naturwissenschaften::550 | Geowissenschaften
Rainfall
Probabilistic Methods
Precipitation Intensity
Hydraulic engineering
Rain
Amazonian
Geography
Planning and Development

Madeira River
Biochemistry
Suspended Sediments
ddc:550
Atlantic Ocean
Groundwater
Clocks
Baseflow
Water Science and Technology
purl.org/pe-repo/ocde/ford#1.05.09 [http]
geography.geographical_feature_category
Base flow
Groundwater Resources
Hydrological Years
Rating Curve
Suspended Sediment
Suspended Sediment Concentrations
ddc:333.7
Sedimentation
Geology
Bolivia
Surface suspended sediment concentrations
Andes
Rating curve
Aquatic Science
Structural basin
Probabilistic Analysis
purl.org/pe-repo/ocde/ford#1.05.00 [http]
Aerodynamics
Rainfall Variability
Hydrology (agriculture)
Rivers
Tributary
Beni River
Counter-clockwise
Dewey Decimal Classification::300 | Sozialwissenschaften
Soziologie
Anthropologie::330 | Wirtschaft::333 | Boden- und Energiewirtschaft::333
7 | Natürliche Ressourcen
Energie und Umwelt

Probability
Hydrology
geography
Hysteresis
Brasil
Amazon River
Sediment
Fluvial Deposit
Concentration (composition)
surface suspended sediment concentrations
Empirical Analysis
purl.org/pe-repo/ocde/ford#1.05.11 [http]
Groundwater Flow
Andean Beni River
Sediment Discharge
ddc:333
7
Zdroj: IGP-Institucional
Instituto Geofísico del Perú
instacron:IGP
Water (Switzerland) 11 (2019), Nr. 12
Water
Volume 11
Issue 12
Repositório Institucional do INPA
Instituto Nacional de Pesquisas da Amazônia (INPA)
instacron:INPA
Popis: Fluvial sediment dynamics plays a key role in the Amazonian environment, with most of the sediments originating in the Andes. The Madeira River, the second largest tributary of the Amazon River, contributes up to 50% of its sediment discharge to the Atlantic Ocean, most of it provided by the Andean part of the Madeira basin, in particular the Beni River. In this study, we assessed the rainfall (R)-surface suspended sediment concentration (SSSC) and discharge (Q)-SSSC relationship at the Rurrenabaque station (200 m a.s.l.) in the Beni Andean piedmont (Bolivia). We started by showing how the R and Q relationship varies throughout the hydrological year (September to August), describing a counter-clockwise hysteresis, and went on to evaluate the R&ndash
SSSC and Q&ndash
SSSC relationships. Although no marked hysteresis is observed in the first case, a clockwise hysteresis is described in the second. In spite of this, the rating curve normally used ( SSSC = aQ b ) shows a satisfactory R2 = 0.73 (p <
0.05). With regard to water discharge components, a linear function relates the direct surface flow Qs&ndash
SSSC, and a hysteresis is observed in the relationship between the base flow Qb and SSSC. A higher base flow index (Qb/Q) is related to lower SSSC and vice versa. This article highlights the role of base flow on sediment dynamics and provides a method to analyze it through a seasonal empirical model combining the influence of both Qb and Qs, which could be employed in other watersheds. A probabilistic method to examine the SSSC relationship with R and Q is also proposed.
Databáze: OpenAIRE