Name: energy loss in food chains
Uploaded: 2025-10-23T11:48:54.000Z
Duration: 46 s
Channel: JoVE

K12 Standards

north-carolina-k-12-science-standard-course-of-study

NC K-12 Science Standard Course of Study

9-12

Earth and Environmental Science

Earth's Systems

ESS.EES.3.4

Trophic Efficiency

- [Anlatıcı] Enerji, bir eko sistemdeki trofik katmanlarda gezinirken, büyük kısmı ısı şeklinde kaybolur.
 Enerji bir formdan ötekine döner.
 Termodinamiğin ikinci kuralı.
 Ilıman bir orman eko sisteminde birincil üreticilerden birincil tüketicilere sunulan enerji yaklaşık yılde metrekare başına 6000 kilokaloridir.
 Ancak bir sonraki trofik tabakada, birincil tüketiciler bu orijinal miktarın ancak %10'unu kullanabilirler.
 Bu enerji transfer ölçümüne trofik katman transfer verimliliği ya da TLTE denir ve genellikle de, üst katmanları desteklemeye yetecek enerji olmadığından, bir ekosistemdeki besin zincirlerinin uzunluğunu sınırlayan en temel faktördür.

Tucker, Marlee A. ve Tracey L. Rogers. "Deniz ve Karasal Memelilerde Avcı-Av Vücut Büyüklüğü, Trofik Seviyesi ve Vücut Kütlesinin İncelenmesi." Royal Society B Bildirileri: Biyolojik Bilimler 281, no. 1797 (22 Aralık 2014). [<a href="https://doi.org/10.1098/rspb.2014.2103" target="__blank">Kaynak</a>]

Sanders, Dirk, Andrea Moser, Jason Newton ve F. J. Frank van Veen. "Trofik asimilasyon verimliliği, dört seviyeli konakçı-parazitoid besin zincirinde daha yüksek trofik seviyelerde belirgin şekilde artar." Royal Society B Bildirileri: Biyolojik Bilimler 283, no. 1826 (16 Mart 2016). [<a href="https://doi.org/10.1098/rspb.2015.3043" target="__blank">Kaynak</a>]

trofik verimlilik

Trofik seviye transfer verimliliği (TSTV), bir trofik seviyeden diğerine toplam enerji transferinin bir ölçüsüdür. Metabolik ısı olarak kaybedilen enerji nedeniyle, üretilen enerjinin ortalama yalnızca %10'u bir sonraki seviyeye aktarılır. Bu enerji kaybı modeli, bir gıda zincirindeki olası trofik seviye sayısını ciddi şekilde sınırlamaktadır.

<h4>Trofik Seviye Transfer Verimliliği</h4>

Termodinamiğin ikinci yasasına göre, ekosistemden ve bir trofik seviyeden diğerine transfer edilip dönüştürülürken büyük miktarda enerji kaybedilir. Biyolojik sistemlerde, bu enerji solunum sırasında metabolik ısı olarak kaybolur. Bir trofik seviyeden diğerine enerji transferinin ölçümü, trofik seviye transfer verimliliği (TSTV) olarak bilinir ve mevcut trofik seviyedeki ve önceki seviyedeki enerji üretiminin bir fonksiyonudur. Bu ölçüm, besin zincirlerinin toplam uzunluğu ile ilgili geniş sonuçlara sahiptir. 

<h4>"10'lar Kuralı"</h4>

Genel olarak, enerjinin yalnızca %10'u bir trofik seviyeden diğerine aktarılır ve bu değer ekosisteme bağlı olarak %5-20 arasında değişebilir. Bu, elde edilen enerjinin %90'ının her trofik seviyede kaybedildiği ve ekosistemdeki mümkün olan maksimum seviye sayısını büyük ölçüde etkilediği anlamına gelir. Örneğin, bir ekosistem güneşten 600.000 Kcal güneş enerjisi aldıysa, birincil üreticiler otçullara yalnızca 60.000 Kcal aktarılacak, bu da ikincil tüketicilere yalnızca 6.000 Kcal, üçüncül tüketicilere 600 Kcal ve besin zincirinin tepesindeki dördüncül tüketicilere 60 Kcal altarılacaktır. Günde ortalama 2000 Kcal'a ihtiyaç duyan bir kurt gibi apeks bir avcı, günlük kalori kotasını karşılamak için çok yüksek miktarda ikincil veya üçüncül tüketici tüketmelidir.

Trofik Verimlilik

Trofik seviye transfer verimliliği (TLTE), bir trofik seviyeden diğerine toplam enerji transferinin bir ölçüsüdür. Gibi yoğun enerji kaybı nedeniyle ...

Education

JoVE Core

Biology

Biyoloji

Ecology

Ekoloji

Ecosystems

Ekosistemler

KEY TERMS AND CONCEPTS

TEMEL TERİMLER VE KAVRAMLAR

energy loss in food chains

Trophic level transfer efficiency describes how much energy moves from one level of a food chain to the next. It shows why energy drops sharply as organisms eat and are eaten. In most ecosystems, only about 10% of the energy passes on.

This energy loss follows the second law of thermodynamics. In living systems, much of the energy is lost as metabolic heat during respiration. Trophic level transfer efficiency, or TLTE, measures this transfer by comparing the energy produced at one trophic level with the energy available from the previous level.

The 10% rule is a useful guide, although the transfer can range from about 5% to 20% depending on the ecosystem. That means about 90% of the energy is lost at each step. This loss limits how many trophic levels a food chain can support.

A simple energy example shows the pattern. If an ecosystem received 600,000 Kcal of solar energy, primary producers would pass only 60,000 Kcal to herbivores. Those herbivores would pass 6,000 Kcal to secondary consumers, then 600 Kcal to tertiary consumers, and 60 Kcal to quaternary consumers.

This energy shortage also affects top predators. A wolf, for example, needs about 2000 Kcal per day. To meet that need, it would have to eat a large number of secondary or tertiary consumers.

Energy Loss in Food Chains

what is an ecosystem?

Ecosystem Zones and Climate

Ecosystems are shaped by living and nonliving parts of an environment, and they can be grouped as terrestrial or aquatic. Terrestrial ecosystems depend on climate. Aquatic ecosystems are divided into freshwater and marine systems, and depth affects water temperature and how much sunlight reaches the water. Terrestrial ecosystems are called biomes. A biome is defined by climate and by the organisms that live there. Near the equator, rainforests have high, aseasonal temperatures and high annual...

trophic levels

Food Chains and Energy Flow

Food chains show how energy and nutrients move through an ecosystem. Each organism holds a trophic level, or a specific place in that chain. The lowest level includes primary producers, which make their own food using energy from the sun or from chemicals. Organisms at the next levels are heterotrophs, which get energy from other organisms below them. Primary consumers are herbivores, and they feed on autotrophs, also called primary producers. Secondary and tertiary consumers are carnivores...

primary production

GPP, NPP, and Ecosystem Energy

Gross primary production and net primary production describe how energy enters and moves through ecosystems. Primary producers, or autotrophs, make their own food. They can do this by photosynthesis or chemosynthesis, and they can also gain energy by consuming other organisms. The rate at which producers capture and store this energy is called gross primary production, or GPP. Not all of the energy in GPP stays available to the rest of the ecosystem. Primary producers use some energy for...

production efficiency

Energy Transfer as Biomass Efficiency

Net production efficiency shows how much energy organisms turn into biomass for the next trophic level. It focuses on the usable energy stored in body tissue, not the energy lost as heat or excreted wastes. This makes it a key idea for understanding energy flow through ecosystems. As energy moves from one organism to the next, only biomass can serve as food for the next trophic level. The rest of the energy is used in metabolism and is lost over time. Net production efficiency, or NPE, is the...

trophic efficiency

Trophic level transfer efficiency describes how much energy moves from one level of a food chain to the next. It shows why energy drops sharply as organisms eat and are eaten. In most ecosystems, only about 10% of the energy passes on. This energy loss follows the second law of thermodynamics. In living systems, much of the energy is lost as metabolic heat during respiration. Trophic level transfer efficiency, or TLTE, measures this transfer by comparing the energy produced at one trophic...

what are biogeochemical cycles?

Nutrient Recycling in Ecosystems

Nutrient recycling in ecosystems keeps the elements needed for life moving through living and nonliving parts of the environment. Elements such as water, carbon, nitrogen, sulfur, and phosphorus are present in limited amounts, so they must be conserved and reused. These movements are called biogeochemical cycles. These nutrients can exist in several chemical forms. They may spend long periods in the atmosphere, on land, under the land, or in aquatic environments. Decomposition is a key part of...

the water cycle

Water Movement Through Earth Systems

Water movement through Earth systems connects the hydrosphere, the atmosphere, the land, and living things. The hydrosphere includes every place where water is stored or moves. Because water supports living processes, its movement is important for ecosystem dynamics. The cycle starts when the sun warms surface water on land and in the oceans. That water evaporates and enters the atmosphere as vapor. Water can also move into the air by sublimation, which is ice changing directly into vapor, and...

the carbon cycle

Carbon Movement in Living Systems

Carbon moves through living systems and Earth over short and long time scales. It is the basis of all organic matter on Earth, and it cycles through ecosystems by passing between organisms and by moving through rocks, oceans, and the atmosphere. Human activities, including farming and burning fossil fuels, have changed this balance. In the biological carbon cycle, carbon dioxide in the atmosphere reacts with water to form bicarbonate. Primary producers, or autotrophs, use carbon dioxide and...

the nitrogen cycle

Nitrogen in Soil and Living Things

Nitrogen in soil and living things moves through ecosystems in several forms. Nitrogen atoms are found in proteins and DNA. Most animals and plants cannot use nitrogen gas, which is the main form of nitrogen on Earth. Nitrogen must first be changed into a usable form by nitrogen-fixing bacteria before it can move through food webs. About 78% of the air we breathe is nitrogen gas, but few organisms can use it in that form. Nitrogen fixation changes nitrogen gas (N2) into ammonia (NH3).

the phosphorus cycle

Phosphorus Movement in Soil and Water

Phosphorus moves through ecosystems mostly as phosphate ions in soil, water, sediment, and rocks. Unlike carbon, water, and nitrogen, it is not found in the atmosphere as a gas. It is also often a limiting nutrient, which means it is in short supply in many environments. Phosphorus is important in DNA, cell membranes, bones, and teeth. It is found in minerals, sediment, volcanic ash, and aerosols. As rocks and sediment weather over time, they release inorganic phosphate. That phosphate then...

the sulfur cycle

Sulfur in Ecosystems and Acid Rain

Sulfur moves through ecosystems as part of the chemical cycle that supports life. It is an important element in proteins and in amino acids such as cysteine, which helps give proteins their structure. On land, sulfur reaches ecosystems in several ways. Weak sulfuric acid can fall with precipitation, sulfur can drop directly from the atmosphere, rocks can weather and release sulfur, and geothermal vents can add it as well. Plants and microorganisms take sulfur up from the soil and change it...

bioremediation

Bioremediation in Soil and Oil Cleanup

Bioremediation uses prokaryotes, fungi, or plants to remove pollutants from the environment. It is a practical way to reduce harmful chemicals in contaminated soil and water. In agriculture, fertilizers and pesticides can leach into groundwater, streams, and lakes. Microbes and bacteria can help break down these toxins. One example is atrazine, an environmental toxin found in many fertilizers, which can be removed from soils by the bacterial species Rhizobium and Tricoderma sp. Bioremediation...

key terms and concepts

Learn how trophic level transfer efficiency limits food chains, why only about 10% of energy moves upward, and how heat loss affects top predators.

Energy Loss in Food Chains | JoVE K12

JoVE Core series brings biology to life through over 300 concise and easy-to-understand animated video lessons that explain key concepts in biology, plus more than 150 scientist-in-action videos that show actual research experiments conducted in today’s laboratories.

biology

JoVE Core serisi, biyolojinin ana konseptlerini açıklayan 300 adet kısa ve kolay anlaşılabilir olan video dersleriyle ve günümüz laboratuvarlarında yürütülen gerçek araştırmaları gösteren 150'den fazla \"bilim insanları iş başında\" videolarıyla biyolojiye hayat vermektedir.

Pennsylvania State Academic Standards

Life Science

interdependent-relationships-in-ecosystems

Interdependent Relationships in Ecosystems

3.1.9-12.I

matter-and-energy-in-organisms-and-ecosystems

Matter and Energy in Organisms and Ecosystems

3.1.9-12.F

3.1.9-12.H

Louisiana Student Standards for Science

High School

Life Sciences

from-molecules-to-organisms-structures-and-processes

From Molecules To Organisms: Structures And Processes

HS-LS1-7

ecosystems-interactions-energy-and-dynamics

Ecosystems: Interactions, Energy And Dynamics

HS-LS2-1

HS-LS2-4

Environmental Science

Tennessee Academic Standards

Ecosystems: Interactions, Energy, and Dynamics

BIO1.LS2.4

Virginia  Standards of Learning

HIgh School

BIO.8

BIO.8.b

LS.5

LS.5.b

Physical Science

PS.5

PS.5.b

new-jersey-student-learning-standards-for-science

New Jersey Student Learning Standards for Science

Arizona Science Standards

HS.L2

HS.L2U1.19

Alabama Course of Study Science

Ecosystems: Interactions Energy and Dynamics

9-12.B.2.6

9-12.EVS.1.1

Next Generation Science Standards

HS-LS2-6

Florida Department of Education

SC.912.L.17

SC.912.L.17.9

Texas Essential Knowledge and Skills

BIO.13

BIO.13.B

Georgia Standards of Excellence

Botany

SBO6.

All Standards

south-carolina-college-and-career-ready-science-standards

South Carolina College and Career Ready Science Standards

B-LS2-1.

B-LS2-2.

Earth and Space Science (ESS)

Earth’s Systems

E-ESS2-2.

E-ESS2-3.

SEV1.

SEV1.d

new-york-state-science-learning-standards

New York State Science Learning Standards

HS-LS2-3.

HS-LS2-4.

Oceanography

SO3.

SO3.2

SEC4.

SEC4.d

SB5.b

myJoVE Corporation

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Use models to explain how mantle convection powers plate tectonics.

ESS.EES.2.1

Analyze and interpret data to predict locations of volcanoes and earthquakes based on plate boundaries.

ESS.EES.2.2

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Use models to explain how plate tectonics influence topography.

ESS.EES.2.3

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Conditions on Early Earth

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The Water Cycle

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The Nitrogen Cycle

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The Phosphorus Cycle

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The Sulfur Cycle

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Bioremediation

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Carry out investigations to explain how the rock cycle and rates of weathering, erosion, and soil formation influence Earth's systems.

ESS.EES.2.4

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What is Weather?

Overview

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Variation of Atmospheric Pressure

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Analyze and interpret data to explain how volcanic activity influences changes in Earth's atmosphere, geosphere, biosphere, and hydrosphere.

ESS.EES.2.5

States of Water

Water exists in any one of the three classical states: solid (ice), liquid (water), and gas (steam or water vapor). The state of water depends on i) the ...

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Solvents

A solvent is a substance, most often a liquid, that can dissolve other substances. Here, the substance being dissolved is called a solute. When a solvent ...

Carry out investigations to explain the properties of water.

ESS.EES.3.1

Analyze how the geosphere is shaped by plate tectonics and the rock cycle.

Energy Loss in Food Chains

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