@article{fdi:010069273, title = {{M}easuring and modeling vertical gradients in suspended sediments in the {S}olimoes/{A}mazon {R}iver}, author = {{A}rmijos, {E}. and {C}rave, {A}. and {E}spinoza, {R}. and {F}raizy, {P}ascal and {D}os {S}antos, {A}lmr and {S}ampaio, {F}. and {D}e {O}liveira, {E}. and {S}antini, {W}illiam and {M}artinez, {J}ean-{M}ichel and {A}utin, {P}. and {P}antoja, {N}. and {O}liveira, {M}. and {F}ilizola, {N}.}, editor = {}, language = {{ENG}}, abstract = {{A}ccurately measuring sediment flux in large rivers remains a challenge due to the spatial and temporal cross-sectional variability of suspended sediment concentrations in conjunction with sampling procedures that fail to accurately quantify these differences. {T}his study presents a field campaign methodology that can be used to improve the measurement of suspended sediment concentrations in the {A}mazon {R}iver or similarly large rivers. {T}he turbidity signal and {R}ouse model are together used in this study to define the spatial distribution of suspended sediment concentrations in a river cross-section, taking into account the different size fractions of the sediment. {W}ith this methodology, suspended sediment fluxes corresponding to each sediment class are defined with less uncertainty than with manual samples. {T}his paper presents an application of this methodology during a field campaign at different gauging stations along a 3,000-km stretch of the {S}olimoes/{A}mazon {R}iver during low water and flood periods. {V}ertical concentration profiles and {R}ouse model applications for distinctive sediment sizes are explored to determine concentration gradients throughout a cross-section of the river. {T}he results show that coupling both turbidity technology and the {R}ouse model may improve our understanding of the spatial distribution of different sediments fractions sizes in the {S}olimoes/{A}mazon {R}iver. {T}hese data are very useful in defining a pertinent monitoring strategy for suspended sediment concentrations in the challenging context of large rivers.}, keywords = {in situ concentration measurement ; {R}ouse model ; {S}olimoes ; {A}mazon {R}iver ; suspended sediments ; turbidity ; {PEROU} ; {BRESIL} ; {AMAZONE} ; {SOLIMOES} {COURS} {D}'{EAU}}, booktitle = {}, journal = {{H}ydrological {P}rocesses}, volume = {31}, numero = {3}, pages = {654--667}, ISSN = {0885-6087}, year = {2017}, DOI = {10.1002/hyp.11059}, URL = {https://www.documentation.ird.fr/hor/fdi:010069273}, }