TY - JOUR
T1 - Influence of near-bottom re-suspended sediment on benthic light availability
AU - Pedersen, Troels Møller
AU - Gallegos, Charles L.
AU - Nielsen, Søren Laurentius
PY - 2012
Y1 - 2012
N2 - Increased light attenuation in the water column is a common consequence of the increased organic loading that accompanies anthropogenic eutrophication in coastal systems. Frequently, the best water quality correlate of the light attenuation coefficient is the total suspended solids, even in systems in which nutrient loading occurs primarily by groundwater input, that is, without strong river inputs of sediment. Alteration of bottomsediment texture, organic content, and bulk density by organic loading has been well documented. Here we report the effect of sedimentre-suspension on near-bottomlight attenuation using an array of in situ light sensors with very close spacing near the sediment–water interface and a radiative transfer (RT) modeling with the software “Hydrolight”. We found that the light attenuation coefficient over 4.5 cm just above the bottom exceeded the attenuation found higher in the water column by a factor ranging from 1.6 to >30. RT modeling indicated that light received at the bottom could be overestimated by a factor 4 or more by extrapolating measurements not taking the near-bottomlight attenuation into account. The results may help explain the wide range of seagrass light requirements observed in different systems.
AB - Increased light attenuation in the water column is a common consequence of the increased organic loading that accompanies anthropogenic eutrophication in coastal systems. Frequently, the best water quality correlate of the light attenuation coefficient is the total suspended solids, even in systems in which nutrient loading occurs primarily by groundwater input, that is, without strong river inputs of sediment. Alteration of bottomsediment texture, organic content, and bulk density by organic loading has been well documented. Here we report the effect of sedimentre-suspension on near-bottomlight attenuation using an array of in situ light sensors with very close spacing near the sediment–water interface and a radiative transfer (RT) modeling with the software “Hydrolight”. We found that the light attenuation coefficient over 4.5 cm just above the bottom exceeded the attenuation found higher in the water column by a factor ranging from 1.6 to >30. RT modeling indicated that light received at the bottom could be overestimated by a factor 4 or more by extrapolating measurements not taking the near-bottomlight attenuation into account. The results may help explain the wide range of seagrass light requirements observed in different systems.
KW - light attenuation
KW - radiative transfer modeling
KW - seagrass distribution
KW - sediment organic content
KW - turbidity
U2 - 10.1016/j.ecss.2012.04.027
DO - 10.1016/j.ecss.2012.04.027
M3 - Journal article
SN - 0272-7714
VL - 106
SP - 93
EP - 101
JO - Estuarine, Coastal and Shelf Science
JF - Estuarine, Coastal and Shelf Science
ER -