Important Formulas Flashcards

(42 cards)

1
Q

Lincoln Index

A

A statistical measure used to estimate population sizes, calculated as (E1)(E2)/S.

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2
Q

Population Growth Rate (PGR)

A

Calculated by (Number of Births - Number of Deaths)/(Total Population Size), indicating how quickly a population is expanding or contracting.

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3
Q

Energy Conversion

A

1 kJ = 1000 Joules; 1 kcal = 1000 calories; 1 calorie = 4.184 joules.

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4
Q

Power formula

A

Calculated as Power = Energy/Time.

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5
Q

Population Growth Rate (percentage)

A

Calculated as (Births - Deaths) / Total Population x 100, indicating percentage change in a population.

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6
Q

Percent Change formula

A

(New Value - Old Value) / Old Value x 100, calculating the percentage difference between two values.

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7
Q

Rule of 70 formula

A

70 / Growth Rate, used to estimate the time for a population to double.

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8
Q

Population Density formula

A

Total Population / Land Area, measuring the number of individuals in a specific area.

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9
Q

Efficiency formula

A

Energy Output / Energy Input x 100, indicating the percentage of energy conversion.

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10
Q

Rate of Change formula

A

Final - Initial / Final time - Initial time, measuring the change over time.

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11
Q

Gross Primary Productivity (GPP)

A

GPP = Total solar energy captured by plants − Energy lost due to respiration.

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12
Q

Net Primary Productivity (NPP)

A

NPP = Gross primary productivity (GPP) - Respiration.

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13
Q

The 10% Rule

A

Only approximately 10% of energy transfers between trophic levels in a food chain.

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14
Q

Dimensional Analysis

A

Quantity 1 x (Conversion factor / Quantity 2 ) = Result, used to convert units.

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15
Q

Half-Life formula

A

t½ = ln (2) / λ, where t1/2 is the half-life and λ is the decay constant.

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16
Q

Respiration equation

A

C6H12O6 + 6O2 → 6CO2 + 6H2O, the process by which organisms convert glucose into energy.

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17
Q

Combustion reaction

A

Hydrocarbons (CxHy) + O2 → CO2 + H2O, representing the burning of hydrocarbons.

18
Q

Photosynthesis equation

A

6CO2 + 6H2O + sunlight → C6H12O6 + 6O2, the process through which plants convert light energy into chemical energy.

19
Q

Ocean Acidification equation

A

CO2 + H2O ↔ H2CO3 ↔ H+ + HCO3-, demonstrating the chemical reactions involved in ocean acidification.

20
Q

Photochemical Smog Formation

A

NOx + VOCs + heat + sunlight → smog, describing the reaction that leads to smog formation.

21
Q

Stratospheric Ozone Depletion equation

A

O3 + Cl → O2 + ClO, representing the chemical reaction responsible for ozone layer depletion.

22
Q

A statistical measure used to estimate population sizes, calculated as (E1)(E2)/S.

A

Lincoln Index

23
Q

Calculated by (Number of Births - Number of Deaths)/(Total Population Size), indicating how quickly a population is expanding or contracting.

A

Population Growth Rate (PGR)

24
Q

1 kJ = 1000 Joules; 1 kcal = 1000 calories; 1 calorie = 4.184 joules.

A

Energy Conversion

25
Calculated as Power = Energy/Time.
Power formula
26
Calculated as (Births - Deaths) / Total Population x 100, indicating percentage change in a population.
Population Growth Rate (percentage)
27
(New Value - Old Value) / Old Value x 100, calculating the percentage difference between two values.
Percent Change formula
28
70 / Growth Rate, used to estimate the time for a population to double.
Rule of 70 formula
29
Total Population / Land Area, measuring the number of individuals in a specific area.
Population Density formula
30
Energy Output / Energy Input x 100, indicating the percentage of energy conversion.
Efficiency formula
31
Final - Initial / Final time - Initial time, measuring the change over time.
Rate of Change formula
32
GPP = Total solar energy captured by plants − Energy lost due to respiration.
Gross Primary Productivity (GPP)
33
NPP = Gross primary productivity (GPP) - Respiration.
Net Primary Productivity (NPP)
34
Only approximately 10% of energy transfers between trophic levels in a food chain.
The 10% Rule
35
Quantity 1 x (Conversion factor / Quantity 2 ) = Result, used to convert units.
Dimensional Analysis
36
t½ = ln (2) / λ, where t1/2 is the half-life and λ is the decay constant.
Half-Life formula
37
C6H12O6 + 6O2 → 6CO2 + 6H2O, the process by which organisms convert glucose into energy.
Respiration equation
38
Hydrocarbons (CxHy) + O2 → CO2 + H2O, representing the burning of hydrocarbons.
Combustion reaction
39
6CO2 + 6H2O + sunlight → C6H12O6 + 6O2, the process through which plants convert light energy into chemical energy.
Photosynthesis equation
40
CO2 + H2O ↔ H2CO3 ↔ H+ + HCO3-, demonstrating the chemical reactions involved in ocean acidification.
Ocean Acidification equation
41
NOx + VOCs + heat + sunlight → smog, describing the reaction that leads to smog formation.
Photochemical Smog Formation
42
O3 + Cl → O2 + ClO, representing the chemical reaction responsible for ozone layer depletion.
Stratospheric Ozone Depletion equation