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  2. Ferrocement - Wikipedia

    en.wikipedia.org/wiki/Ferrocement

    Ferrocement or ferro-cement [1] is a system of construction using reinforced mortar [2] or plaster (lime or cement, sand, and water) applied over an "armature" of metal mesh, woven, expanded metal, or metal-fibers, and closely spaced thin steel rods such as rebar. The metal commonly used is iron or some type of steel, and the mesh is made with ...

  3. Earth's internal heat budget - Wikipedia

    en.wikipedia.org/wiki/Earth's_internal_heat_budget

    Primordial heat is the heat lost by the Earth as it continues to cool from its original formation, and this is in contrast to its still actively-produced radiogenic heat. The Earth core's heat flow—heat leaving the core and flowing into the overlying mantle—is thought to be due to primordial heat, and is estimated at 5–15 TW. [23]

  4. Ferropericlase - Wikipedia

    en.wikipedia.org/wiki/Ferropericlase

    Ferropericlase or magnesiowüstite is a magnesium/iron oxide with the chemical formula (Mg,Fe)O that is interpreted to be one of the main constituents of the Earth's lower mantle together with the silicate perovskite ((Mg,Fe)SiO 3), a magnesium/iron silicate with a perovskite structure. Ferropericlase has been found as inclusions in a few ...

  5. Ground vibrations - Wikipedia

    en.wikipedia.org/wiki/Ground_vibrations

    Ground vibrations is a technical term that is being used to describe mostly man-made vibrations of the ground, in contrast to natural vibrations of the Earth studied by seismology. For example, vibrations caused by explosions, construction works, railway and road transport, etc. - all belong to ground vibrations.

  6. Iron cycle - Wikipedia

    en.wikipedia.org/wiki/Iron_cycle

    The iron cycle is an important component of the terrestrial ecosystems. The ferrous form of iron, Fe 2+, is dominant in the Earth's mantle, core, or deep crust. The ferric form, Fe 3+, is more stable in the presence of oxygen gas. [22] Dust is a key component in the Earth's iron cycle.

  7. Geophysics - Wikipedia

    en.wikipedia.org/wiki/Geophysics

    The Earth is cooling, and the resulting heat flow generates the Earth's magnetic field through the geodynamo and plate tectonics through mantle convection. [13] The main sources of heat are: primordial heat due to Earth's cooling and radioactivity in the planets upper crust. [14] There is also some contributions from phase transitions.

  8. 2002 Indian heat wave - Wikipedia

    en.wikipedia.org/wiki/2002_Indian_heat_wave

    In some areas, temperatures were so extreme that many tin-roofed homes turned into ovens, water catchments dried up and animals collapsed from the heat. [8] Heatwave in 2002 led not only to a very high mortality rate, but also to the high morbidity of many heat-related diseases and caused a fatal blow to the local agriculture and economy.

  9. Ferrocerium - Wikipedia

    en.wikipedia.org/wiki/Ferrocerium

    A modern ferrocerium firesteel product is composed of an alloy of rare-earth metals called mischmetal, containing approximately 20.8% iron, 41.8% cerium, about 4.4% each of praseodymium, neodymium, and magnesium, plus 24.2% lanthanum. [5] A variety of other components are added to modify the spark and processing characteristics. [2]

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