This work aims to study the phenomenon of scaling observed in the hot water pipelines in the southern seaside touristic installations of Agadir city. This phenomenon has led to the formation of solid deposits and adherents to the internal walls of the facilities of the hot water. This deposit is at the origin of several technical, economic and environmental problems. It causes a decrease in the lifetime of boilers and a reduction of thermal exchanges and consequently a decrease in the energy efficiency of heating systems. In the present study, the samples of scale have been carried out at different points of hot water pipelines. The characterization of different scale samples recovered was conducted by X-ray fluorescence (XRF), elemental analysis (CHNS-O), infrared spectrometry (IR), thermogravimetric analysis (TGA), differential thermal analysis (DTA), X-ray diffraction (XRD) and scanning electron microscopy (SEM). Analytical results showed that scale samples collected on different sites in touristic hot water system are mostly formed by calcium carbonate. Thermodynamic conditions in the site were favourable to the aragonite variety formation.
The region of Souss Massa occupies an important place in the touristic industry of Morocco both by its natural and cultural riches as well as by its performance in the tourism sector. Agadir city remains the first destination of the Kingdom by a hotel capacity of 27,542 beds approximately. Touristic installations offer 16% of jobs in the region [
Agadir city is served with water from groundwater sources. Wells and boreholes produce on average 250 l/s and superficial (stations for the treatment of Sidi Boushab 300 l/s and that of Tamri 700 l/s supplied respectively by the waters of the Dams Abdelmoumen and Moulay Abdellah. The hotel sector which has consumed 2265.103 m3 of water in 2014 [
The present work has for object the identification and characterization of deposits of scale formed in hot water pipelines in the south of the touristic area of Agadir. The samples of scale have been carried out at different points. Well distributed according to the standardized methods. Several analytical techniques were used: elemental analysis CHNS-O, XRF, IR, DTA, TGA, XRD and SEM.
Agadir city is located on the shore of the Atlantic Ocean near the foot of the western High Atlas Mountains. The collection of the Scale has been made at the level of different installations of hot water in the southern seaside touristic establishments of Agadir located at coordinates: (30.39, −9.59) (
X-Ray Fluorescence (XRF) analyses are performed on a PAN Analytical Axios. The applied voltage is 60 kV with a current of 125 mA and Power 4.103 W.
Infrared spectroscopy (IR) analysis is carried out with Bruker FTIR-ATR vertex model 70, with a resolution of 4 cm−1 in 16 scans to collect the data in an interval ranging from 4.102 to 4.103 cm−1. The samples are placed directly on the ATR crystal (Diamond of reflection). The mode used is the “total reflectance attenuated” (ATR).
X-ray diffraction analysis was done using the appliance PAN Analytical using a diffractometer type X-Pert-Pro with an anode material of copper and a monochromator of Cu-Kα radiation (λ = 1.5406 Å). The applied voltage is 45 kV with a current of 40 mA at 25˚C. The sample morphologies are directly examined by scanning electron microscopy (SEM) using a FEG Zeiss Supra running at an accelerating voltage of 3 kV to limit load on the sample. The thermogravimetric analysis (TGA) and differential thermal analysis (DTA) were carried out on a thermal analyser (DTG-60), under air from 0˚C to 1100˚C to heating rate of 10˚C/min. The Elementary Analysis CHNS/O is carried out with 2000 Flash EA 1112, thermo Fisher Scientific. Software used: EAGER 300.
The qualitative analysis by X-ray fluorescence (XRF) was used to identify the chemical elements in the scale samples.
XRF quantitative analysis results are presented in
The calcium oxide (CaO) is the major oxide in scale samples. It represents 52.07 wt%. Other oxides are also detected with very low contents. The silica (SiO2) and magnesium
oxide (MgO) present respectively a percentage of 1.10% and 0.94% in weight. Other oxides in state of traces have been detected like sulphuric oxide SO3 (0.32%), phosphorus pentoxide P2O5 (0.22%), sodium oxide Na2O (0.20%), iron oxide Fe2O3 (0.11%), aluminium oxide (Al2O3) (0.09%).
The Elemental chemical Analysis CHNS/O has been conducted to determine the percentage of the mass of Carbon, Hydrogen, Nitrogen, Sulphur or Oxygen in the scale samples.
The hydrogen and sulphur elements are present with very low percentages which are respectively 0.35% and 0.17%. The nitrogen element has not been detected as seen at
The analysis by IR spectroscope has given the results presented in
The thermal decomposition of sample is shown in
Compound | Weight % |
---|---|
Calcium oxide (CaO) | 52.07 |
Silica (SiO2) | 1.10 |
Magnesium oxide (MgO) | 0.94 |
Sulphuric oxide (SO3) | 0.32 |
Phosphorus pentoxide (P2O5) | 0.22 |
Sodium oxide (Na2O) | 0.20 |
Iron Oxyde (Fe2O3) | 0.11 |
Aluminumoxide (Al2O3) | 0.09 |
Potassium Oxide (K2O) | 0.00 |
Element | C | H | N | S | O |
---|---|---|---|---|---|
Weight % | 10.70 | 0.35 | 0.00 | 0.17 | 49.68 |
and lattice water. Whereas, the endothermic peak at 800˚C is attributed to the decomposition of calcium carbonate CaCO3 to CaO and CO2. TGA analysis curve show a total mass loss of 41%:8% loss of surface and lattice water between 0˚C to 300˚C and 33% at high temperature associated to the elimination of vapors such as CO2 generated by the decomposition of calcium carbonate. These observations are in agreement with the literature data (39% to 43% for a temperature between 500˚C and 700˚C and the 44% as theoretical value) [
The peaks which include 2θ = 27.5˚, 33.5˚ and 45.9˚ correspond to the calcium carbonates of the aragonite type which is metastable to the ordinary temperature and which is formed at a temperature above 60˚C [
The scale samples analysis with the scanning electron microscopy (SEM) has given results as we can see at
The use of various analytical techniques has allowed us to identify and characterize the solid deposits found in the internal walls of hot water pipes in the south of the touristic area of the Agadir city.
Quantitative analysis results showed that calcium carbonates amount exceeds 93 wt%. The carbonates anion has been well identified in the infra-red spectrum. The process of decomposition of calcium carbonates has been highlighted by the quantitative analysis by XRF. The calcium oxide CaO represents 52% of the scale weight. Thermal analysis results confirmed this result and showed the calcium carbonate decomposition process. The crystal structure of the scale is the aragonite variety as it has been determined by X-ray diffraction. Micrographs obtained by scanning electronic microscope confirm this structure.
Indeed, the scale deposited in the hot water system is mostly formed of calcium carbonate. Due to temperature, particles of calcium carbonate were crystallized under the aragonite variety. These results will allow us to focus our research of suitable inhibitors of scaling in order to prevent the deposit of scale in the hot water system in the touristic area in Agadir city.
Belattar, M., Ben- Aazza, S., Aba-Aaki, R., Hadfi, A., Hafid, N., Boukbir, L. and Driouiche, A. (2016) Contribution to the Study of Hot Water Scaling Phenomenon in the South of Touristic Area in Agadir City. Journal of Water Resource and Protection, 8, 1035-1043. http://dx.doi.org/10.4236/jwarp.2016.812082