Primary Productivity of lakes and rivers 1.) Of whole water columns (no container) Diurnal O 2 method 2.) Of phytoplankton (bottles in situ) Dark and light.

Slides:



Advertisements
Similar presentations
AP Lab #12 Dissolved Oxygen & Aquatic Primary Productivity part I
Advertisements

Photosynthesis & Primary Production. Photosynthesis Solar energy powers the reaction Carbon dioxide and water used to make glucose Oxygen gas is released.
Primary Production measurements over a daily cycle in Clark’s Cove Ayan Chaudhuri, Lin Zhang, Anne-Marie Brunner MAR640 – Global Marine Biogeochemistry.
Aquatic Productivity and Dissolved O2 lab
Light – life energy source. Light absorbed, reflected and transmitted.
Section Percent Composition and Chemical Formulas
MOLES! MOLES! MOLES! Joe’s 2 nd Rule of Chemistry.
PRIMARY PRODUCTIVITY Productivity is the rate of biomass formation Primary productivity (photosynthesis) of phytoplankton can be measured directly by O.
Dissolved oxygen and aquatic primary productivity.
Properties of Light in Water Refraction Attenuation with depth Light and Trophic Status Secchi Disk Application.
AP BIO Lab 12 Dissolved Oxygen. OXYGEN AVAILABILITY Depends on: ~Temperature: Ability to hold oxygen decreases as water temp gets warmer ~ Photosynthetic.
Dissolved Oxygen. Photosynthesis: Your one-stop shop for all of your oxygen needs! Carbon Dioxide (from air) Water (from ground) Oxygen (to air) Carbohydrate.
SUSANNA SCOTT MIAMI UNIVERSITY Ecosystem Metabolism: Response to Storm Events.
Ocean Productivity Kelp Forest Macroalgae: 3% of Ocean Photosynthesis
PRIMARY PRODUCTIVITY Productivity is the rate of biomass formation Primary productivity (photosynthesis) of phytoplankton can be measured directly by O.
mgC/m3/d 1.0 primary production decreases at highest light intensity o
An undisturbed sediment core containing varves from the deposition zone of a deep lake The varves can be used to calculate dates along the core profile.
“The open ocean is a biological desert.”. Primary Production Global chlorophyll concentrations for Oct
OC211(OA211) Phytoplankton & Primary Production Dr Purdie SOC (566/18) LECTURE 6 Week 6 (i) Photosynthesis & Light (ii) Critical.
OC211(OA211) Phytoplankton & Primary Production Dr Purdie SOC (566/18) LECTURE 5 Week 5 (i) Measuring Primary Production: The.
10 Productivity and Food Webs in the Sea Notes for Marine Biology: Function, Biodiversity, Ecology By Jeffrey S. Levinton ©Jeffrey S. Levinton 2001.
Phytoplankton Dynamics Primary Productivity (g C/m 2 /yr) Gross (total) production = total C fixed Net production = C remaining after respiration Standing.
Properties of Gas in Water Oxygen Sources and Sinks Oxygen Distribution (space & time) Measuring Dissolved Oxygen Measuring 1º Production and Respiration.
Dissolved Oxygen and Primary Productivity Lab
Open Oceans: Pelagic Ecosystems II
Lab 12: Dissolved Oxygen Description –measure primary productivity by measuring O 2 production –factors that affect amount of dissolved O 2 temperature.
Measuring Solubility Chapter 11. Solubility  The solubility of a substance refers to the maximum amount of that substance that can be dissolved in a.
Water as an Environment Oxygen Profiles Light Part 2.
Phytoplankton bloom – there is no officially recognized threshold level –range from 10,000s – 1,000,000s of cells per ml.
Ecosystem Productivity. Assessment Statements 2.5.2: Describe photosynthesis and respiration in terms of inputs, outputs and energy transformations :
Temperature Measured with a thermometer Units are ◦C
Dissolved Oxygen and Aquatic Primary Productivity
1 Example A 25.0  L sample was found to contain 26.7  g glucose. Express the concentration as ppm and mg/dL glucose. Solution A ppm is defined as  g/mL,
Nutrient Cycles in Marine Ecosystems Part I Section 4.
% by Mass Another way to measure the concentration of a solution % by mass = mass solute x 100 mass solution Solution = solute + solvent.
Ch. 9. Aquatic ecosystems and Physiology: Energy Flow  Productivity  Dissolved Oxygen Fig Hypothetical Trophic Structure Model. Boxes are filled.
Section 10.3 Percent Composition and Chemical Formulas.
Fig. 14-CO, p Fig. 14-1a, p. 382 Fig. 14-1b, p. 383.
Ch. 3 Ecosystems GPP & NPP. The amount of energy available in an ecosystem determines how much life an ecosystem can support.
Aquatic Biomes Chapter 10 Section 1. An aquatic habitat is one in which the organisms live in or on water. Aquatic biomes and their ecosystems are scattered.
Solutions. Classification of Matter Solutions are homogeneous mixtures.
Comparison of light in six New York lakes Amanda Davis Lauren Jetty Jennifer Mokos Justen Walker.
Epipelagic Zone.
Patterns of Ecosystem Metabolism Ruhl Student Center, Community Room
PRIMARY PRODUCTIVITY Productivity is the rate of biomass formation
1 Photosynthesis and Cellular Respiration. 2  Photosynthesis is the anabolic pathway in which light energy from the sun is converted to chemical energy.
Topic 6. 5 Solutions. Solutions are homogeneous mixtures. The most common way to express solution concentration is by molarity.
PRIMARY PRODUCTIVITY Productivity is the rate of biomass formation Primary productivity (photosynthesis) of phytoplankton can be measured directly by O.
Ecosystem Productivity
The Mole Honors Chem. -How do we measure chemical quantities? -What units of measure do we use?
Dissolved oxygen (DO) in the streams
Is the Primary production is the rate of synthesis of organic material from inorganic compounds such as CO 2 and water. It is significant in that it provides.
Tides and Intertidal zones. First a Review Get your oceanography toolbox out Let’s try to fill in the parts.
Solution Concentration.  Lesson Objectives  Describe the concept of concentration as it applies to solutions, and explain how concentration can be increased.
Lab 12 Dissolved Oxygen. Dissolved oxygen indicates water quality  Air contains 95% more oxygen than water  Water’s ability to hold dissolved oxygen.
AP BIO Lab 12 Dissolved Oxygen. OXYGEN AVAILABILITY Depends on: ~Temperature: Ability to hold oxygen decreases as water temp gets warmer ~ Photosynthetic.
Sources of Oxygen Demand in the Lower San Joaquin River, California
Primary Productivity.
Primary Productivity: Dissolved Oxygen “DO”
Primary Production measurements over a daily cycle in Clarks Cove
Dissolved Oxygen Maslyn, AP Biology.
CC9 - Calculating Involving Masses (p26-30)
Measuring Productivity of a System: Explained!
Chapter 11 – Measuring Solubility
Aquatic Ecosystems.
AQA GCSE QUANTITATIVE CHEMISTRY 1
What is Productivity? Amount of solar energy provided to an ecosystem
Molar Conversions (p.80-85, )
Concentrations of Solutions
PRIMARY PRODUCTION.
Presentation transcript:

Primary Productivity of lakes and rivers 1.) Of whole water columns (no container) Diurnal O 2 method 2.) Of phytoplankton (bottles in situ) Dark and light bottle O2 method 14 C uptake method

Mid-day Nightime Depth m mg/L O Depth m mg/L O Dashed line 100% O 2 saturation Oxygen profiles for lake water columns –daytime vs nighttime

Dark and light bottle technique for phytoplankton primary production

Van Dorn water sampler—encloses a water sample from a given depth

Changes in Dissolved Oxygen Water samples from various depths are enclosed in light (transparent) and dark (completely opaque) 1 L bottles, For each depth initial readings of dissolved O 2 are taken (IB) and the light (LB) and dark (DB) samples are incubated for a period long enough to produce measurable changes in O 2. During the incubation, we expect that the initial DO concentration (IB) at a given depth will decrease to a lower concentration in the dark bottles (DB) due to respiration of phytoplankton. Conversely, we expect light bottle (LB) should increase from their initial values (IB).

Calculations Gross photosynthesis = [(LB - DB) * 1000 * 0.375] / (PQ *  t) Net photosynthesis = [(LB - IB) * 1000 * 0.375] / (PQ *  t) Respiration = [(IB - DB) * RQ * 1000 * 0.375] /  t Gross and net photosynthesis and respiration are expressed as mg C/m 3 /h LB, DB, and IB are dissolved oxygen concentrations in mg/L  t is the incubation period in hours 1000 converts L to m 3 (1 L = 1000 cm 3 ) converts mass of oxygen to mass of carbon and is a ratio of moles of carbon to moles of oxygen (12 mg C/32 mg O 2 = 0.375)

The Secchi disk—a simple way to estimate light extinction

Light extinction --Light enters from above and its intensity (I) is sharply attenuated with depth (z)—absorption by water or solute molecules or scattered by particles IzIz z Photic zone z 50% z 1% z 10% Section 10.6 Page 144 in text

o o o o mgC/m 3 /d m Depth profile of photosynthesis—how to obtain areal estimate from volumetric 1.0 o Low light intensity, low primary production medium light intensity, highest primary production primary production decreases at highest light intensity