Universal water refers to water in its purest form, free from impurities and contaminants.
Water formation, water isotopes fraction, and the global water cycle are key concepts in understanding the hydrosphere system.
Learning objectives of the lecture include defining "water", discussing some basic concepts and fundamental about the hydrosphere system, and understanding the global water cycle and demand.
Water is a noun, a transparent, odorless, tasteless liquid, a compound of hydrogen and oxygen, H2O, freezing at 0 ° C and boiling at 100 ° C, in more or less impure state.
Transpiration is represented as T.
Groundwater is represented as s.
Land Surface is represented as g.
Groundwater Flow is represented as G.
Evaporation is represented as E.
Infiltration is represented as I.
Storage is represented as s.
Subsurface Flow is represented as Rg.
Surface Runoff is represented as R.
Precipitation is represented as P.
Unsteady Flow Equation: I = Input (volume/time) O= Output (volume/time) dS/dt = Time rate of change of storage.
Water (H2O) is the general systematic name for water, also known as Aqua, Hydrogen oxide, Dihydrogen monoxide, Hydrogen hydroxide, Oxane, Oxidane, and Molecular name H2O.
The molar mass of water (H2O) is 18.0153 g/mol.
Water appears as a transparent, almost colorless liquid with a slight hint of blue.
A simple hydrologic system model is one where what goes in, goes out.
A watershed is represented as a system boundary.
These components can be grouped into subsystems of the overall cycle to analyze the total system, with the simpler subsystems treated separately and the results combined according to the interactions.
The hydrologic cycle may be treated as a system whose components are precipitation, evaporation, runoff and other phases in the hydrologic cycle.
A hydrologic system is defined as a structure or volume in space, surrounded by a boundary, that accepts water and other inputs, operates on them internally, and produces them as outputs.
To describe relationships between different variables in the hydrologic cycle, the input, I, is represented as precipitation and the output, Q, is represented as runoff.
In the absence of perfect knowledge, the components of the hydrologic cycle can be represented in a simplified way by means of the system concept.
The input to a watershed is represented as rainfall.
The output from a watershed is represented as streamflow, which includes evaporation and subsurface flow.
The storm rainfall-runoff process on a watershed can be represented as a hydrologic system.
There are 8 billion people in 2022, 5.3 billion in 1900, 6.1 billion in 2000, 2050, and 2100.
Water scarcity will affect hundreds of millions of people by 2100.
Water is life's mater and matrix, mother and medium, and there is no life without water, according to Albert Szent-Györgyi, a Nobel Prize Winner in Medicine in 1937.
Factors affecting demand for water include population growth, industrial and rural development/land uses, water charges, and consumer preferences.
There are also stable oxygen atoms with 17 or 18 nucleons (one or two extra neutrons) written as 17 O and 18 O.
Nature has provided us with something almost as good as paint in the form of isotopes.
Hydrogen comes in three flavors: 1 H (usually written as simply H), 2 H (D, or deuterium) and 3 H (T, or tritium, which is radioactive).
Tritium was released to the atmosphere during the test phase for hydrogen bombs.
The radioactive isotope tritium (3 H) and the stable isotopes deuterium (2 H) and oxygen-18 (18 O) are rare components of the water molecule H 2 O.
Tracking the movements of water through the system — in oceans, air, clouds, rain, snow, ice, lakes, rivers, and back to the oceans — is a primary concern of climatologists.
The most abundant isotope of water is H 2 16 O, but the isotopes H 2 18 O and HD 16 O are also relatively common and can be easily measured.
In computer models, it is relatively easy to "paint" different water masses different colors and then see how the "red" water spreads around the system.