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As we stated earlier, the Dead Sea is
a terminal lake which receives its inflow from the Jordan
River in the north, from a few perennial springs and streams
and from flash floods cascading down the mountain ravines.
It has no outflow, with the dry heat of the Dead Sea region
water slowly evaporating into the Air, leaving some of the
salts in certain conditions to accumulate in the lake. This
has produced one of the saltiest lakes in the world with an
average salinity of 345g/l of salt per liter water, compared
with the ocean’s 35g/l.}
The Sea of Life™'s (Dead Sea)
location and its salinity make it a rare natural source for
balneo/thalasso treatments which have been recognized for
centuries.
The brine of the Dead Sea contains a unique array of salts,
enriched with Magnesium, Sodium, Potassium, Calcium, Bromine,
Iron, Selenium, Zinc and relatively high concentrations of
trace elements. The water has a high specific gravity and
great buoyancy, making it easy to float on its surface.
The unique composition of the brine
derives from the evaporation of seawater via the crystallization
of the minerals, the addition of salts from land sources,
the weathering of rocks and the the dissolution of trace elements.
The brine also contains high concentrations of trace elements.
| |
| Chloride |
212.400,0 |
| Bromide |
5.120,0 |
| Bicarbonate |
220,0 |
| Sulphate |
470,0 |
| Sodium |
39.1450,0 |
| Potassium |
7.260,0 |
| Calcium |
16.860,0 |
| Magnesium |
40.650,0 |
Thermo-mineral Water:
According to Eckstein, there are many natural mineral springs
and seepages in the area, as follows:
| Name |
Water Temperature (0C) |
| Ein Hakikar |
28,5 |
| Ein Tamar (Arus) |
29,5 |
| Ein Mumileh |
30,0 |
| Hammei Zohar Hot Springs |
31.0 |
| Ein Nurit |
39.0 |
| Hammei Mazor (Ein Gedi) |
40.5 |
| Hammei Shalem |
44.5 |
| Ein Tureiba |
30.0 |
| Ein Ehwher |
29.0 |
| Ein Feschcha (Zukim) |
29.0 |
| Ein Chazal |
29.0 |
Two of these hot water springs are currently
being exploited: Hammei Zohar (Zohar Hot Springs) and Hammei
Mazor (Ein Gedi Hot Springs).
Hammei Zohar (Zohar Hot Springs)
The Zohar Hot Springs are located on the south-western shore
of the Dead Sea.
The springs feed four spa facilities
close by, which in turn offer a range of balneological services.
Salinity and temperature depend on the depth from which the
water is drilled.
The table below is a chemical analysis of Hammei Zohar spring
water.
| |
| |
Surface |
Borehole 56 m |
Depth 148 m |
| Temp.°C |
28-31 |
32 |
34,5 |
| PH |
6,1 |
|
|
| Fluoride |
0.35 |
0.2 |
1.3 |
| Chloride |
35,509.5 |
84,960.0 |
139,500.0 |
| Bromide |
769.5 |
1,910.0 |
3,390.0 |
| Iodide |
0.41 |
1.0 |
4.5 |
| Nitrate |
0,46 |
|
|
| Bicarbonate |
185.5 |
177.0 |
183.0 |
| Sulphate |
677.5 |
747.0 |
830.0 |
| Ammonium |
|
2.08 |
0.26 |
| Lithium |
3.66 |
5.0 |
10.9 |
| Sodium |
8,595.0 |
17,110.0 |
22,200.0 |
| Potassium |
825.0 |
2,075.0 |
3,640.0 |
| Calcium |
3,600.0 |
7,300.0 |
14,000.0 |
| Magnesium |
5,830.0 |
16,000.0 |
26,000.0 |
| Strontium |
52.5 |
140.0 |
270.0 |
| Iron (total) |
|
0.14 |
0.8 |
| Manganese |
0.63 |
6.26 |
4.80 |
| Metasilicic Acid
|
21,7 |
|
|
| Carbon dioxide |
|
|
421,0 |
| Hydrogen sulphide |
9.0 |
12.0 |
16.0 |
| Radon Rn 222 |
6700 |
707 |
610 |
| Radon Ra 226 |
23 |
40.6 |
18.2 |
The water of the hot springs differs
from the water of the Dead Sea and the
balneological potentials differ as well.
Water analysis of the drill indicates a high content of magnesium,
sodium and calcium. The main anion was chloride and also included
sulfate and bicarbonate. Analysis also showed a high concentration
of the following trace elements: bromide, iodine, lithium,
strontium and magnesium. A high content of hydrogen sulfide
was also found.
Hammei Mazor (Ein Gedi Hot Springs)
The water at the Hammei Mazor (Ein Gedi
Hot Springs) are drilled from a depth of 48 meters underground.
The temperature of the water at the drill measured 400C (104
F).
The table below is based on the analysis
conducted by K.E. Quentin.
| One kg. of the water sample contains: |
| |
Mass Milligram |
Equivalent
Millimol |
Equivalent
% |
| |
| Sodium(NA+) |
23170 |
1007,83 |
43,15 |
| Kalium (K+) |
2620 |
67,01 |
2,87 |
| Ammonium (NH4+) |
0,53 |
0,03 |
--- |
| Calcium (CA2+) |
7950 |
396,71 |
16,99 |
| Magnesium (Mg2+) |
10500 |
864,02 |
36,99 |
| Mangan (Mn2+) |
0,27 |
0,01 |
--- |
| Total: |
44.240,80 |
1.335,61 |
100,00 |
| |
| |
| Fluoride (F-) |
1,27 |
0,07 |
--- |
| Chloride (Cl-) |
81,900 |
2310,10 |
98,01 |
| Bromide (Br-) |
1590 |
19,90 |
0.84 |
| Iodine (I-) |
1,05 |
0,01 |
--- |
| Sulphate (SO42-) |
1150 |
23,96 |
1,02 |
| Hydrogensulphide
(HS-) |
7,93 |
0,24 |
0,01 |
| Hydrogencarbonate
(HCO3-) |
169 |
2,77 |
0,12 |
| Hydrogenphosphate
(HPO42-) |
0,41 |
0,01 |
--- |
| Total |
84.819,76 |
2.357,06 |
100,00 |
| |
| |
| Flint acid (Metallic)
(H2SiO3) |
26,7 |
|
|
| Total dissolved
minerals: |
129.087,26 |
|
|
| |
| |
| Carbon dioxyde
(CO2) |
245 |
|
|
| Oxygen (O2) |
0,36 |
|
|
| Hydrogen Sulphide
(H2S) |
20,6 |
|
|
| Total for
all dissolved materials: |
129.353,22 |
|
|
| |
| One kg of this
water contains: |
| Element |
Microgram/Kilogram
=mcg/kg |
| Arsen (As) |
1 |
| Cadmium (Cd) |
0,1 |
| Chrome (Cr) |
10 |
| Copper (Cu) |
59 |
| Mercury (Hg) |
0,1 |
| Selenium (Sc) |
1 |
| Lead (Pb) |
11 |
| Zinc (Zn) |
45 |
| Cobalt (Co) |
23 |
| Nickel (Ni) |
27 |
| Molybden (Mo) |
10 |
| Vanadium (V) |
100 |
| Zinc (Sn) |
10 |
| Silver (Ag) |
1 |
The main cautions found were magnesium,
sodium and calcium with large quantities of trace elements
such as bromide, iodine, strontium and manganese. Chloride
is the main anion. General salinity was 13g/kg. The water
contained a high concentration of hydrogen sulphide.
Thanks to the balneo-therapeutic properties of the sulphides
in the thermo-mineral springs, the Dead Sea area has become a world-famous bathing facility and spa.
It is known for the treatment of rheumatic diseases including
muscular and soft tissue rheumatism, discopathies and other
spinal column complaints.
The health facilities in the area offer thermo-mineral waters
by means of pools and baths.
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