Hydrostatic Densitometer for Monitoring Density in Freshwater to Hypersaline Water Bodies

Density, temperature, salinity, and hydraulic head are physical scalars governing the dynamics of aquatic systems. In coastal aquifers, lakes, and oceans, salinity is measured with conductivity sensors, temperature is measured with thermistors, and density is calculated. However, in hypersaline brin...

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Main Authors: Ziv Mor, Hallel Lutzky, Eyal Shalev, Nadav G. Lensky
Format: Article
Language:English
Published: MDPI AG 2021-07-01
Series:Water
Subjects:
Online Access:https://www.mdpi.com/2073-4441/13/13/1842
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spelling doaj-691810eb82504de788cd0a0ae7afa9502021-07-15T15:48:35ZengMDPI AGWater2073-44412021-07-01131842184210.3390/w13131842Hydrostatic Densitometer for Monitoring Density in Freshwater to Hypersaline Water BodiesZiv Mor0Hallel Lutzky1Eyal Shalev2Nadav G. Lensky3Geological Survey of Israel, Jerusalem 9692100, IsraelGeological Survey of Israel, Jerusalem 9692100, IsraelGeological Survey of Israel, Jerusalem 9692100, IsraelGeological Survey of Israel, Jerusalem 9692100, IsraelDensity, temperature, salinity, and hydraulic head are physical scalars governing the dynamics of aquatic systems. In coastal aquifers, lakes, and oceans, salinity is measured with conductivity sensors, temperature is measured with thermistors, and density is calculated. However, in hypersaline brines, the salinity (and density) cannot be determined by conductivity measurements due to its high ionic strength. Here, we resolve density measurements using a hydrostatic densitometer as a function of an array of pressure sensors and hydrostatic relations. This system was tested in the laboratory and was applied in the Dead Sea and adjacent aquifer. In the field, we measured temporal variations of vertical profiles of density and temperature in two cases, where water density varied vertically from 1.0 × 10<sup>3</sup> kg·m<sup>−3</sup> to 1.24 × 10<sup>3</sup> kg·m<sup>−3</sup>: (i) a borehole in the coastal aquifer, and (ii) an offshore buoy in a region with a diluted plume. The density profile in the borehole evolved with time, responding to the lowering of groundwater and lake levels; that in the lake demonstrated the dynamics of water-column stratification under the influence of freshwater discharge and atmospheric forcing. This method allowed, for the first time, continuous monitoring of density profiles in hypersaline bodies, and it captured the dynamics of density and temperature stratification.https://www.mdpi.com/2073-4441/13/13/1842hydrostatic densitometerdensity measurementhypersaline brinecoastal aquiferfresh–saline water interfacediluted plume
collection DOAJ
language English
format Article
sources DOAJ
author Ziv Mor
Hallel Lutzky
Eyal Shalev
Nadav G. Lensky
spellingShingle Ziv Mor
Hallel Lutzky
Eyal Shalev
Nadav G. Lensky
Hydrostatic Densitometer for Monitoring Density in Freshwater to Hypersaline Water Bodies
Water
hydrostatic densitometer
density measurement
hypersaline brine
coastal aquifer
fresh–saline water interface
diluted plume
author_facet Ziv Mor
Hallel Lutzky
Eyal Shalev
Nadav G. Lensky
author_sort Ziv Mor
title Hydrostatic Densitometer for Monitoring Density in Freshwater to Hypersaline Water Bodies
title_short Hydrostatic Densitometer for Monitoring Density in Freshwater to Hypersaline Water Bodies
title_full Hydrostatic Densitometer for Monitoring Density in Freshwater to Hypersaline Water Bodies
title_fullStr Hydrostatic Densitometer for Monitoring Density in Freshwater to Hypersaline Water Bodies
title_full_unstemmed Hydrostatic Densitometer for Monitoring Density in Freshwater to Hypersaline Water Bodies
title_sort hydrostatic densitometer for monitoring density in freshwater to hypersaline water bodies
publisher MDPI AG
series Water
issn 2073-4441
publishDate 2021-07-01
description Density, temperature, salinity, and hydraulic head are physical scalars governing the dynamics of aquatic systems. In coastal aquifers, lakes, and oceans, salinity is measured with conductivity sensors, temperature is measured with thermistors, and density is calculated. However, in hypersaline brines, the salinity (and density) cannot be determined by conductivity measurements due to its high ionic strength. Here, we resolve density measurements using a hydrostatic densitometer as a function of an array of pressure sensors and hydrostatic relations. This system was tested in the laboratory and was applied in the Dead Sea and adjacent aquifer. In the field, we measured temporal variations of vertical profiles of density and temperature in two cases, where water density varied vertically from 1.0 × 10<sup>3</sup> kg·m<sup>−3</sup> to 1.24 × 10<sup>3</sup> kg·m<sup>−3</sup>: (i) a borehole in the coastal aquifer, and (ii) an offshore buoy in a region with a diluted plume. The density profile in the borehole evolved with time, responding to the lowering of groundwater and lake levels; that in the lake demonstrated the dynamics of water-column stratification under the influence of freshwater discharge and atmospheric forcing. This method allowed, for the first time, continuous monitoring of density profiles in hypersaline bodies, and it captured the dynamics of density and temperature stratification.
topic hydrostatic densitometer
density measurement
hypersaline brine
coastal aquifer
fresh–saline water interface
diluted plume
url https://www.mdpi.com/2073-4441/13/13/1842
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AT hallellutzky hydrostaticdensitometerformonitoringdensityinfreshwatertohypersalinewaterbodies
AT eyalshalev hydrostaticdensitometerformonitoringdensityinfreshwatertohypersalinewaterbodies
AT nadavglensky hydrostaticdensitometerformonitoringdensityinfreshwatertohypersalinewaterbodies
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