(আবহাওয়া

Noun:

সমদ্বিবাহু ত্রিভুজ,

isotherm শব্দের বাংলা অর্থ এর উদাহরণ:

আর কেবল দুই বাহু সমান হলে তাকে সমদ্বিবাহু ত্রিভুজ এবং তিনটি বাহুই সমান হলে তাকে সমবাহু ত্রিভুজ বলা হয় ।

একটি চরম সমদ্বিবাহু ত্রিভুজ যার কোণগুলো সোনালি অনুপাতের (Φ:1) বৈশিষ্ট্যযুক্ত ।

সমদ্বিবাহু ত্রিভুজে ।

সমদ্বিবাহু ত্রিভুজ 1 2 b a 2 − b 2 4 = b 4 4 a 2 − b 2 {\displaystyle {\frac {1}{2}}b{\sqrt ।

সমদ্বিবাহু ত্রিভুজের শীর্ষকোণ ।

BCD ত্রিভুজের দুই বাহু সমান, তাই এটি একটি সমদ্বিবাহু ত্রিভুজ ।

সমদ্বিবাহু ত্রিভুজ - যার যে-কোন দুইটি বাহুর দৈর্ঘ্য সমান ।

isotherm's Usage Examples:

To date, 15 different isotherm models have been developed.

The first mathematical fit to an isotherm was published by Freundlich and Kuster.

Therefore, all points through which an isotherm passes have the same or equal temperatures at the time indicated.

An isotherm at 0 °C is called the freezing level.

explains adsorption by assuming an adsorbate behaves as an ideal gas at isothermal conditions.

whichever isotherm is being used is classified as "hot arid" (BWh), and a location with the appropriate temperature below the given isotherm is classified.

The Freundlich equation or Freundlich adsorption isotherm, an adsorption isotherm, is an empirical relationship between the quantity of a gas adsorbed.

whichever isotherm is being used is classified as hot semi-arid (BSh), and a location with the appropriate temperature below the given isotherm is classified.

The Gibbs adsorption isotherm for multicomponent systems is an equation used to relate the changes in concentration of a component in contact with a surface.

_{r}S^{\ominus },} where S is the entropy of the system, with the Gibbs free energy isotherm equation: Δ r G ⊖ = − R T ln ⁡ K e q , {\displaystyle \Delta _{r}G^{\ominus.

the linear adsorption isotherm, which formally resembles Henry's law; therefore, it is also called Henry's adsorption isotherm.

The Langmuir isotherm and Freundlich isotherm are useful in describing this equilibrium.

The freezing level, or 0 °C (zero-degree) isotherm, represents the altitude in which the temperature is at 0 °C (the freezing point of water) in a free.

graphically by a curve, the so-called moisture sorption isotherm.

For each humidity value, a sorption isotherm indicates the corresponding water content value.

This line approximates the 0 °C (32 °F) January isotherm and the 800 millimetres (30 in) isohyet in China.

interface is measured during the compression, a compression isotherm is obtained.

This isotherm shows the variation of surface pressure ( Π = γ o − γ {\displaystyle.

warm air mass, and is typically located on the equator-facing edge of an isotherm gradient.

The northernmost tree line roughly follows the isotherm at the boundary of this region.

Both dehydration and partial melting occurs along the 1,000 °C (1,830 °F) isotherm, generally at depths of 65 to 130 km (40 to 81 mi).

from a to c); this portion of the isotherm corresponds to the liquid-vapor equilibrium.

The regions of the isotherm from a–d and from c–e are interpreted.

From Langmuir's adsorption isotherm, molecules cannot adsorb on surfaces when the adsorption sites are already.

isotherm's Meaning':

(meteorology