enow.com Web Search

Search results

  1. Results from the WOW.Com Content Network
  2. Physical properties of soil - Wikipedia

    en.wikipedia.org/wiki/Physical_properties_of_soil

    Soil temperature depends on the ratio of the energy absorbed to that lost. [68] Soil has a mean annual temperature from -10 to 26 °C according to biomes. [69] Soil temperature regulates seed germination, [70] breaking of seed dormancy, [71] [72] plant and root growth [73] and the availability of nutrients. [74]

  3. Soil - Wikipedia

    en.wikipedia.org/wiki/Soil

    Most living things in soils, including plants, animals, bacteria, and fungi, are dependent on organic matter for nutrients and/or energy. Soils have organic compounds in varying degrees of decomposition, the rate of which is dependent on the temperature, soil moisture, and aeration.

  4. Q10 (temperature coefficient) - Wikipedia

    en.wikipedia.org/wiki/Q10_(temperature_coefficient)

    The Q 10 temperature coefficient is a measure of temperature sensitivity based on the chemical reactions. The Q 10 is calculated as: = / where; R is the rate T is the temperature in Celsius degrees or kelvin. Rewriting this equation, the assumption behind Q 10 is that the reaction rate R depends exponentially on temperature:

  5. Soil thermal properties - Wikipedia

    en.wikipedia.org/wiki/Soil_thermal_properties

    The single probe method employs a heat source inserted into the soil whereby heat energy is applied continuously at a given rate. The thermal properties of the soil can be determined by analysing the temperature response adjacent to the heat source via a thermal sensor. This method reflects the rate at which heat is conducted away from the probe.

  6. Arrhenius equation - Wikipedia

    en.wikipedia.org/wiki/Arrhenius_equation

    In physical chemistry, the Arrhenius equation is a formula for the temperature dependence of reaction rates.The equation was proposed by Svante Arrhenius in 1889, based on the work of Dutch chemist Jacobus Henricus van 't Hoff who had noted in 1884 that the van 't Hoff equation for the temperature dependence of equilibrium constants suggests such a formula for the rates of both forward and ...

  7. Soil respiration - Wikipedia

    en.wikipedia.org/wiki/Soil_respiration

    Carbon is stored in the soil as organic matter and is respired by plants, bacteria, fungi and animals. When this respiration occurs below ground, it is considered soil respiration. Temperature, soil moisture and nitrogen all regulate the rate of this conversion from carbon in soil organic compounds to CO 2. Many methods are used to measure soil ...

  8. AOL Mail

    mail.aol.com

    Get AOL Mail for FREE! Manage your email like never before with travel, photo & document views. Personalize your inbox with themes & tabs. You've Got Mail!

  9. Chemical kinetics - Wikipedia

    en.wikipedia.org/wiki/Chemical_kinetics

    The effect of temperature on the reaction rate constant usually obeys the Arrhenius equation = / (), where A is the pre-exponential factor or A-factor, E a is the activation energy, R is the molar gas constant and T is the absolute temperature. [8]