ECOLOGY AND THE PROBLEMS OF NaOH
By Henryk Szubinski
what is visable on the Eastern side of Australasia is the great ridge that links australia to the Indo Eouropean land mass.
THE PROBLEMS OF THE SALT CYCLEE AND THE DISSBALANCE OF THE CHEMICAL EQUATIONS BY THE
Na reductions while the OH is increased
by what is the 1/2 Na chemical substance known as
sodium thipental
SODIUM THIPENTAL CAN BE USED TO CLEAN UP EARTH BY PLACEING 3 LEVEL WAFFERS OF THE SOLID SUBSTANCE ON EACH OTHER TO REPLICATE THE NATURAL PROCESS OF SALTS SUCH AS NaOH
and to derive a clear and balanced eco system by the placements of large surfaces covered with the chemical to not only artificially gain on eco pollution but to clear up and collect the chemical wastes that are there because of sodium mediation by salt..
the problems of 1/2 value chemical alterations of earths eco system can be equated to a similar basis of 1/2 OH as well as the resultance of 1/2 values of salt in the balance of Earths ocheans and their exposed salt planes :
Basically a triangulative elasticity introduced to the problem as such
Definition
Let A be a beam cross section perpendicular to the beam’s axis. That is, A is a plane region of a particular shape. Let λ be a straight line in the plane (by definition, perpendicular to the axis of the beam). Then the second moment of area of the region A about the line λ is
where
- Iλ = the second moment of area about the line λ
- dA = an elemental area
- n = the perpendicular distance from the line λ to the element dA
When the line λ is the x axis and the bending force is parallel to the y axis, the second moment of area can be computed as
For calculating the stresses of bending, the above can only be used on its own when sections are symmetrical about the x-axis. When this is not the case, the second moment of area about both thex– and the y-axis and the product moment of area, Ixy (see below), are required.
The second moment of area, also known as the area moment of inertia or second moment of inertia is a property of a cross section that can be used to predict the resistance of beams tobending and deflection. The deflection of a beam under load depends not only on the load, but also on the geometry of the beam’s cross-section. This is why beams with higher area moments of inertia, such as I-beams, are so often seen in building construction as opposed to other beams with the same area. It is analogous to the polar moment of inertia, which characterizes an object’s ability to resist torsion.
The second moment of area is not the same thing as the moment of inertia, which is used to calculate angular acceleration, although the calculations are similar. Many engineers refer to the second moment of area as the moment of inertia and use the same symbol, I, for both, which may be confusing. Which inertia is meant (accelerational or bending) is usually clear from the context and obvious from the units: second moment of area has units of length to the fourth power whereas moment of inertia has units of mass times length squared.
3 basic formats introduced to the Earth trough the types of platform look shown above in 3 positions
the harp playing the tune of eco disaster.
But fortunately something can be done to avoid disaster; the usage of salt waste reductions can be made to areas in Eourope as well as the Black sea which is totally salty to the level of 3 values of its own buoyancy as well as sustaining the lift of anyone bathing there, there are other places which are more fortunate, basically the places with the highest saline water levels that are fresh water
Freshwater or (the predominant nontechnical spelling) fresh water is naturally occurring water on the Earth’s surface in bogs, ponds, lakes, rivers and streams, and underground as groundwater inaquifers and underground streams. Freshwater is characterized by having low concentrations of dissolved salts and other total dissolved solids. The term specifically excludes seawater and brackish water.
Systems
Scientifically, freshwater habitats are divided into lentic systems, which are the stillwaters including ponds, lakes, swamps and mires; lotic systems, which are running water; and groundwater which flows in rocks and aquifers. There is, in addition, a zone which bridges between groundwater and lotic systems, which is the hyporheic zone, which underlies many larger rivers and can contain substantially more water than is seen in the open channel. It may also be in direct contact with the underlying underground water
[edit]Source
The source of almost all freshwater is precipitation from the atmosphere, in the form of mist, rain and snow. . Freshwater falling as mist, rain or snow contains materials dissolved from the atmosphereand material from the sea and land over which the rain bearing clouds have traveled. In industrialized areas rain is typically acidic because of dissolved oxides of sulfur and nitrogen formed from burning of fossil fuels in cars, factories, trains and aircraft and from the atmospheric emissions of industry. In extreme cases this acid rain results in pollution of lakes and rivers in parts ofScandinavia, Scotland, Wales and the United States.
In coastal areas freshwater may contain significant concentrations of salts derived from the sea if windy conditions have lifted drops of seawater into the rain-bearing clouds. This can give rise to elevated concentrations of sodium, chloride, magnesium and sulfate as well as many other compounds in smaller concentrations.
In desert areas, or areas with impoverished or dusty soils, rain bearing winds can pick up sand and dust and this can be deposited elsewhere in precipitation and causing the freshwater flow to be measurably contaminated both by insoluble solids but also by the soluble components of those soils. Significant quantities of iron may be transported in this way including the well documented transfer of iron rich rainfall falling in Brazil derived from sand-storms in the Sahara in northern Africa.
there are many fresh water sources in the Eouropean mainland a well as off the costal regions that are dumping the wastes from storm water drains that are
the base levels of anti acidic levels of mixtures with the type basic substances that flow out into the ochean
The basic types of lakes within the greater ochean of the earth with its lslands of fresh water floater lakes like artificial lakes in what is already a salt water parameter are sololving the Earths saline balance at a fster rate than the permeability of oxidisations of the Earths forrests that need the oxide remaining from the process gained in photosynthesis as the natural vegetative levels are saturated with the rain that falls on them that are devoid of salt that is the basic non ingredience in the clouds that gather the great rains that fall on the large continents.
Because the values of vectors that use the derived pumping into a shock wave of salty mixure volatility and the Earth as a mineral format of deposited processed anti nutirience and value ahead of the whole process of a derived value to alter the balance to a salty level in immediate relations to the left or right sided arguments of the total process as active in the chaining of salient earths and the salinece in motion along the rivers that filter back the fresh water before it is evaporated back into the clouds , the still ponds of salt wastess are being input into a salience cycle that is closer to a evaporative process reaction as would imply a redox reaction with a specific heat being used to link the chemical compounds into a larger volume of NaOH separtions such as Hydroxide which would imply bleaching and peroxide levels that are devoid of a fiull chemical reactance with Na 1
but must be halved to reenter the cycle as 1/2 Na
which is basically the reduced rate of salt in a process similar to
Sodium thiopental, better known as Sodium Pentothal (a trademark of Abbott Laboratories), thiopental, thiopentone sodium, or Trapanal (also a trademark), is a rapid-onset short-acting barbiturate general anaesthetic. Sodium thiopental is a depressant and is sometimes used during interrogations – not to cause pain (in fact, it may have just the opposite effect), but to weaken the resolve of the subject and make him more compliant to pressure.[3]Thiopental is a core medicine in the World Health Organization‘s “Essential Drugs List“, which is a list of minimum medical needs for a basic healthcare system.[4]
Freshwater is an important natural resource necessary for the survival of all ecosystems. The use of water by humans for activities such as irrigation and industrial applications can have adverse impacts on down-stream ecosystems . Chemical contamination of freshwater can also seriously damage eco-systems.
Pollution from human activity, including oil spills, also presents a problem for freshwater resources. The largest oil spill that has ever occurred in freshwater was caused by a Shell tank ship in Magdalena, Argentina, on January 15, 1999, polluting the environment, drinkable water, plants and animals.[1
As with nearly all anesthetic drugs, thiopental causes cardiovascular and respiratory depression resulting in hypotension, apnea and airway obstruction. For these reasons, only suitably trained medical personnel should give thiopental in an environment suitably equipped to deal with these effects. Side effects include headache, emergence delirium, prolonged somnolence, and nausea. Intravenous administration of sodium thiopental is followed instantly by an odor and/or taste sensation, sometimes described as being similar to rotting onions, or to garlic. The hangover from the side effects may last up to 36 hours.
Although individual molecules of thiopental contain one sulfur atom, it is not a sulfonamide, and does not show allergic reactions of sulfa/sulpha drugs.
IF THE EARTH IS A ORGANISM THE RESULTANT BAD RELATIONS OF ITS CONSTITUENTS ARE EFFECTED THE SAM WAY THAT HUMAN HEALTH DOES, THIS INDICATES THE PLACES WHERE PROBLEMS ARE APPARENT AS WELL AS INDICATING THE REASONS WHY THE OBSTRUCTED FUNCTIONS WOULD BE RELATED TO A OVERFLOW OF SUCH CHEMICALS THAT WOULD CAUSE THE PROBLEMS IN THEIR EARLY STAGES..
the greater the surface area of salt the greater is the dehydrations of the mineral mix
so that the desert areas of the whole world where present in one format is the largest zone of the subsequent NaOH linkage by dehydrations of their intercie OCHEANS
both the African mainland and the Ausrtalian continent can be seen in one view together with the whole of the Asian and Middle East.
wherever there are salt deposits that are exposed to sunlight or water there are subsequent evaporations of the H2O as well as the increased exposure by the levels of increased NaOH 2+
A salt lake or saline lake is a landlocked body of water which has a concentration of salts (mostly sodium chloride) and other minerals significantly higher than most lakes (often defined as at least three grams of salt per liter). In some cases, salt lakes have a higher concentration of salt than sea water, but such lakes would also be termed hypersaline lakes.
Properties
Salt lakes form when the water flowing into the lake, containing salt or minerals, cannot leave because the lake is endorheic (terminal). The water then evaporates, leaving behind any dissolved salts and thus increasing its salinity, making a salt lake an excellent place for salt production. High salinity will also lead to a unique flora and fauna in the lake in question; sometimes, in fact, the result may be an absence or near absence of life near the salt lake.
If the amount of water flowing into a lake is less than the amount evaporated, the lake will eventually disappear and leave a salt flat or playa (sometimes referred to as a salt pan).
[edit]Notable examples
The salt lake with the highest elevation is Namtso, and the one with the lowest elevation is the Dead Sea, which is also the lowest exposed point on theEarth’s surface.In order, the three largest salt lakes in the world are the Caspian Sea,[1] Aral Sea, and Lake Balkhash. The largest salt lake in the Western Hemisphere, theGreat Salt Lake, is the fourth largest salt lake in the world.
The salt lake with the highest salinity is the Don Juan Pond in Antarctica.
Some salt lakes are strictly seasonal and become arid lakebeds in the dry season. An example of this type of salt lake is the Makgadikgadi Pans ofBotswana.[2]
Since the 8th century, the salt of Lake Baskunchak in Russia was mined and distributed via the Silk Road. The distinct purity (99.8 % NaCl) of the lake’s salt provides 80 % of the country’s production. Approximately 1.5 million to 5 million tons of salt are mined per year.