Name: vaporization, boiling, and evaporation
Uploaded: 2019-03-11T09:21:01.000Z
Duration: 1 min 18 s
Channel: JoVE

K12 Standards

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North Carolina K-12 Science Standard Course of Study

9-12

Earth and Environmental Science

Earth's Systems

ESS.EES.3.1

Vaporization

Waporyzacja to przejście z cieczy do gazu lub pary. Na przykład, gdy energia cieplna jest dodawana do wody, osiąga ona temperaturę wrzenia i staje się parą.
Ilość energii potrzebnej do odparowania danej masy cieczy w stałej temperaturze nazywana jest ciepłem parowania.
Parowanie może również zachodzić na powierzchni cieczy w wyniku parowania. Na zewnątrz energia kinetyczna jest często dostarczana przez słońce i wiatr. Jeśli dodana energia przekracza energię sił międzycząsteczkowych, cząsteczki mogą stać się parą.
Parowanie potu jest dla wielu zwierząt ważnym sposobem na ochłodzenie się. Pot składa się głównie z wody. Może pochłaniać ciepło ze skóry, zwiększając energię kinetyczną cząsteczek wody i powodując jej odparowanie z powierzchni skóry. Powoduje to efekt chłodzenia, który pomaga utrzymać temperaturę ciała.
W roślinach parowanie jest niezbędne podczas transpiracji. Woda parująca z powierzchni liści pomaga w przyciąganiu sąsiednich cząsteczek za pomocą kohezji i adhezji, doprowadzając wodę z korzeni do liści.

odparowywanie

Postać fizyczna substancji zmienia się pod wpływem zmiany jej temperatury. Na przykład podniesienie temperatury cieczy powoduje jej odparowanie (przekształcenie w parę). Proces ten nazywa się parowaniem—i jest zjawiskiem powierzchniowym. Aby doszło do parowania, energia kinetyczna musi być większa niż siły międzycząsteczkowe, które utrzymują cząsteczki w wiązaniu. Ilość energii potrzebnej do odparowania pewnej ilości cieczy pod danym ciśnieniem i w stałej temperaturze nazywa się ciepłem parowania. Kiedy woda w stanie ciekłym odparowuje, zamienia się w parę.

Jedną z metod odparowywania jest podgrzewanie cieczy aż do osiągnięcia temperatury wrzenia. Wrzenie następuje, gdy pod powierzchnią cieczy tworzą się pęcherzyki pary. Temperatura wrzenia zmienia się w zależności od ciśnienia atmosferycznego. Przy wyższym ciśnieniu atmosferycznym potrzeba więcej energii, aby osiągnąć temperaturę wrzenia. Na poziomie morza woda wrze w normalnej lub atmosferycznej temperaturze wrzenia (100 ⁰C lub 212 ⁰F). Na większych wysokościach woda potrzebuje mniej energii do wrzenia. Na przykład woda wrze w temperaturze około 71 ⁰C (160 ⁰F) na Mount Everest.

Ewaporacja, inny rodzaj odparowywania, zachodzi poniżej temperatury wrzenia. W tym procesie cząsteczki wody o energii kinetycznej wystarczającej do pokonania sił międzycząsteczkowych uciekają z powierzchni wody w postaci pary. Pozostałe cząsteczki wody mają niższą energię kinetyczną. Jeśli dzieje się to na dużą skalę, całkowita energia kinetyczna masy cieczy maleje, chłodząc ciecz. Pocenie się wykorzystuje zjawisko parowania w celu obniżenia temperatury ciała. Kiedy pot odparowuje z ciała, pozostały pot jest chłodniejszy i pomaga absorbować ciepło z ciała.

Rośliny wykorzystują również właściwości parowania wody, aby pomóc w przemieszczaniu wody w górę przez roślinę. W skali środowiskowej parowanie wody jest silnikiem napędzającym obieg wody oraz znaczną część pogody i klimatu na Ziemi.

Odparowywanie

Fizyczna forma substancji zmienia się poprzez zmianę jej temperatury. Na przykład podniesienie temperatury cieczy powoduje parowanie cieczy ...

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vaporization, boiling, and evaporation

Vaporization changes a liquid into vapor when temperature adds enough kinetic energy to overcome intermolecular forces. It is a surface phenomenon, which means it starts at the liquid’s surface. The energy needed to vaporize a set amount of liquid at a given pressure and constant temperature is called the heat of vaporization.

Water shows this process clearly. When liquid water is vaporized, it becomes steam. One way this happens is boiling, which occurs when vapor bubbles form beneath the surface of the liquid. The boiling point changes with atmospheric pressure. With more pressure, more energy is needed to reach the boiling point.

At sea level, water boils at the normal, or atmospheric, boiling point of 100 °C, or 212 °F. At higher elevations, water needs less energy to boil. For example, water boils at about 71 °C, or 160 °F, on Mount Everest. Evaporation is another form of vaporization, but it happens below the boiling point.

During evaporation, water molecules with enough kinetic energy escape from the surface as vapor. The molecules left behind have lower kinetic energy. If evaporation happens on a large scale, the liquid loses overall kinetic energy and cools. Sweat uses this effect to lower body temperature. As perspiration evaporates, the cooler sweat helps absorb heat from the body. Plants also use water’s evaporative properties to move water upward through the plant. On a larger scale, evaporation drives the water cycle and helps shape Earth’s weather and climate.

Vaporization, Boiling, and Evaporation

the periodic table and organismal elements

the-periodic-table-and-organismal-elements

Periodic Table Basics for Living Things

The periodic table helps explain which elements living things need and how those elements are related. Elements are the smallest units of matter that cannot be broken down further by chemical processes. There are 118 known elements, but not all occur naturally, and even fewer are essential for life. Living matter is made mostly of carbon, nitrogen, hydrogen, and oxygen. Together, these elements make up most of the human body and are also found in all life on Earth. Smaller amounts of calcium,...

atomic structure

Atoms and Their Subatomic Particles

Atoms are the smallest units of elements, and they make up all matter. Each atom contains three subatomic particles: protons, neutrons, and electrons. These particles give an atom its mass and its charge. The idea that matter is made of tiny particles goes back to Democritus, a Greek philosopher around 450 B.C. He used the word atomos, which means “indivisible.” The idea was not accepted at the time, but it returned many centuries later. In the 19th century, John Dalton proposed an atomic...

isotopes

Atomic Mass and Isotope Basics

Atomic mass and isotopes are linked by the number of protons and neutrons in an atom. The number of protons sets an element’s atomic number, or Z. For example, every atom with eight protons is oxygen. Atoms of the same element can still differ because they can have different numbers of neutrons. The mass number, or A, is the total of protons and neutrons. Atoms with the same atomic number but different mass numbers are called isotopes. Elements can have several isotopes. Carbon-12, carbon-13,...

electron behavior

Electron Shells and Valence Electrons

Electrons are negatively charged subatomic particles that occupy regions around the positively charged nucleus of an atom. Their location is linked to energy levels called shells. They are also grouped into sub-shells and orbitals within each shell. An electron’s shell shows its general energy level. Electrons closer to the nucleus have less energy, while electrons farther away have more energy. The sub-shell gives a more exact location and energy level. An orbital is the shape of the region...

electron orbital model

Electron Orbitals and Energy Levels

Electron orbitals show where electrons are most likely to be found around the atomic nucleus. They also help explain energy levels, orbital shapes, and three-dimensional orientation. In an atom, electron location is described first by a shell, or principal energy level. It is then described by a subshell within that shell and by the individual orbitals inside each subshell. The first shell is closest to the nucleus. It has only one subshell and one spherical orbital, called the 1s orbital.

covalent bonds

Electronegativity and Covalent Bond Polarity

Covalent bonds form when two atoms share electrons to fill their valence shells. The way those shared electrons are pulled depends on electronegativity, which is an atom’s ability to attract electrons in a bond. When atoms have similar electronegativities, they form nonpolar covalent bonds. When their electronegativities differ, the bond is polar because the electrons are shared unevenly. The number of covalent bonds an atom can make depends on its valence electrons. Oxygen has six valence...

ionic bonds

Ionic Compounds and Electrolytes

Ionic compounds form when atoms gain or lose electrons to reach a more stable electron configuration. The charged particles that result are called ions. Ionic bonds are electrostatic attractions between oppositely charged ions. The most reactive elements include those with one valence electron, such as potassium, and those that need one more valence electron, such as chlorine. Ions that lose electrons become positive cations. Ions that gain electrons become negative anions. Cations and anions...

hydrogen bonds

Hydrogen Bonds in Water

Hydrogen bonds in water are weak attractions between atoms that are already part of other chemical bonds. One atom is electronegative, such as oxygen, and carries a partial negative charge. The other is a hydrogen atom that is bonded to another electronegative atom and has a partial positive charge. These attractions form because hydrogen has very weak electronegativity when it binds with a strongly electronegative atom like oxygen or nitrogen. The electrons in that bond are shared unequally.

van der waals interactions

Intermolecular Forces in Polar Solutions

Intermolecular forces are the attractions and repulsions that act between atoms and molecules. These electrostatic forces come from particles with permanent, partial, or temporary charges. For neutral atoms and molecules, the main types are ion-dipole, dipole-dipole, and dispersion forces, which are together called van der Waals forces. Polar molecules have a partial positive end and a partial negative end. That separation of charge creates a dipole. In water, oxygen is more electronegative...

elements and compounds

Elements, Compounds, and Bonding

Elements and compounds are the two main kinds of pure substances. A pure substance contains only one kind of matter. An element contains only one type of atom. A compound contains two or more types of atoms joined by a chemical bond. Elements can be atomic or molecular, depending on their basic units. They are unique forms of matter with specific chemical and physical properties. Ordinary chemical reactions cannot break an element into a smaller substance. There are 118 elements, but only 98...

molecular shapes

Electron Geometry and Lone Pairs

Electron geometry and lone pairs help explain why molecules take specific shapes. The arrangement of electron groups around a central atom controls the molecular geometry. Valence electrons form bonding pairs, which sit mainly between bonded atoms, or lone pairs, which belong to one atom only. Electron pairs in the valence shell spread out to reduce repulsion. They do this by maximizing the distance between one another. A diatomic molecule has two regions of electron density, and these are...

pH Scale in Everyday Solutions

pH measures how acidic or basic a water-based solution is. It depends on the concentration of hydronium ions, H3O+, in the solution. In one liter of pure water at neutral pH, there are 1×10−7 moles of hydronium ions. Because hydronium ion levels can vary over a very wide range, measuring pH directly in moles is not practical. The pH scale converts hydronium ion concentration into a negative logarithm. Pure water has a pH of 7 and is neutral. Most solutions fall between 0 and 14, but some, such...

chemical reactions

Atoms, Bonds, and Chemical Reactions

Chemical reactions rearrange atoms to form new substances. In a reaction, the starting materials are called reactants, and the new substances are called products. The atoms stay the same type and number, but their bonds change, so the substances become different compounds. During a chemical reaction, bonds between atoms break and form again. This means the shared electrons are rearranged. Some reactions happen on their own, while others need an energy source such as heat or light. In biology,...

redox reactions

Electron Transfer in Redox

Redox reactions are chemical reactions that involve electron transfer between atoms or molecules. When one particle gains electrons, another must lose them at the same time. That is why oxidation and reduction always happen together. The two roles in a redox reaction are linked. The atom that is oxidized acts as the reducing agent, or reductant. The atom that is reduced acts as the oxidizing agent, or oxidant. A simple way to remember the ideas is OIL-RIG, which means oxidation is losing...

cohesion

Water Molecules and Surface Tension

Water molecules stick to each other through cohesion. Water is neutral overall, but it is a polar molecule. The oxygen atom in one water molecule has a partial negative charge, and it can bind with a hydrogen atom that has a partial positive charge in another water molecule. This forms a hydrogen bond. Each water molecule can form up to four hydrogen bonds with other water molecules, and these bonds give water its cohesive nature. Cohesion helps water form droplets on a surface. Water does not...

adhesion

Water Climbing by Adhesion

Water can climb or stick to surfaces because of adhesion, which is the attraction between different kinds of molecules. In water, this is easy to see on polar surfaces such as glass or cellulose in plants. The positive hydrogen side of water is more attracted to the negative oxygen in silica than to nearby water molecules. This attraction helps explain capillary action. If a narrow glass tube is placed in a beaker of water, water molecules attach to the tube’s surface and the water level rises.

states of water

Water Phase Changes and Ice Density

Water changes between solid, liquid, and gas states as temperature and molecular motion change. In this lesson, the focus is on how water freezes, melts, vaporizes, and returns to liquid or solid form. The balance between intermolecular forces, which pull molecules together, and kinetic energy, which pushes them apart, controls each state. Water freezes when intermolecular forces become stronger than kinetic energy. Unlike most substances, ice is less dense than liquid water. This happens...

specific heat

How Specific Heat Affects Temperature

Specific heat capacity describes how much energy a substance needs to rise by 1 degree Celsius for each gram. It is often written with calories, grams, and degrees Celsius, but it can also be shown in joules, kilograms, and Kelvin. For water, 1 gram needs 1 calorie to increase by 1°C, which is also written as 1 cal/g-°C or 4186 J/kg/K. Water has a high specific heat capacity, so it takes in a large amount of heat before its temperature changes much. It also gives off a lot of heat when it...

vaporization

Vaporization changes a liquid into vapor when temperature adds enough kinetic energy to overcome intermolecular forces. It is a surface phenomenon, which means it starts at the liquid’s surface. The energy needed to vaporize a set amount of liquid at a given pressure and constant temperature is called the heat of vaporization. Water shows this process clearly. When liquid water is vaporized, it becomes steam. One way this happens is boiling, which occurs when vapor bubbles form beneath the...

solvents

Water as a Biological Solvent

Water acts as a biological solvent in many living systems. A solvent is a substance, usually a liquid, that dissolves another substance called a solute. When a solvent and a solute mix, they form a solution, which is a uniform mixture of both parts. Water is called a universal biological solvent because its polar structure helps it dissolve many other polar compounds. Polarity means that one side of the molecule has a slight positive charge and the other side has a slight negative charge.

carbon skeletons

Carbon Backbones in Biomolecules

Carbon backbones give biological molecules their structure and flexibility. Living things are built from macromolecules that contain carbon atoms, and organic compounds are defined by a carbon backbone. Carbon is tetravalent, so each carbon atom can bond with four other atoms. Its valence electrons are stable, so carbon rarely becomes an ion. As carbon chains get longer, they can form ring structures, double bonds, and branching side chains. Carbon-carbon bonds create the carbon skeleton.

key terms and concepts

Explore how heat changes liquids into vapor, including boiling, evaporation, boiling point changes with pressure, cooling from sweat, and the water cycle.

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From Molecules to Organisms: Structures and Processes

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Vaporization, Boiling, and Evaporation

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