Overview of essential concepts related to plant nutrition and nutrient cycling in ecosystems.
Important updates for students:
Practice exam is now available.
Office hours scheduled for tomorrow from 4:45-5:45 PM via Zoom.
Reminder: One week to report any grading mistakes.
Review session on Sunday at 5 PM with Dr. Chapman and Dr. Wieder (Zoom link provided).
Upcoming exam next Monday covering material until Friday's lecture. Students should bring computers.
Wednesday lecture will be in person; next Friday designated for project catch-up.
Topics to be covered in class include:
Plant nutrient limitations and the role of fertilizers.
Eutrophication and its effects.
Overview of nutrient cycling with a Hawaiian case study.
Importance of salmon:
Key fishery for Native American tribes; integral to their lifestyles.
Salmon contribute to fertilizing soils and forests.
Historical challenges:
Logging, dams, water extraction, and pollution have severely reduced wild salmon populations since the 1950s.
Restoration efforts:
Fifty years of research leading towards successful projects aimed at salmon restoration.
Restoration often involves improving water flow to facilitate salmon migration up to 850 miles.
Mechanisms attracting beneficial soil organisms include:
Nitrogen-fixing bacteria and mycorrhizae associations.
Nitrogen fixation requires a conducive environment that is typically provided within rhizobium nodules in legumes.
Energy costs of nitrogen fixation:
Lab conditions illustrate that nitrogen fixation consumes 25% of growth in carbohydrates given to bacteria.
Nitrogen uptake from soil is less costly.
Fertilizer effects:
When inorganic nitrogen is supplied through fertilizers, plants often reduce nitrogen fixation.
Crop rotation practices:
Farmers utilize nitrogen-fixing plants in crop rotations (e.g., corn followed by legumes) to replenish soil nitrogen.
Comparison of agriculture vs. natural ecosystems:
Agriculture depletes soil mineral content, strains water reserves, and encourages erosion.
Natural ecosystems cycle nutrients effectively and restore their own reserves.
Soil conservation strategies aim to reduce agricultural damage:
Implementing no-till agriculture and utilizing cover crops.
Purpose and composition of fertilizers:
Fertilizers are used to supplement nutrient removal in agriculture.
Commercial fertilizers: minerals either mined or synthetically produced (e.g., Haber-Bosch process for nitrogen).
"Organic" fertilizers are made from manure, fishmeal, or compost.
Environmental impacts:
Energy-intensive fertilizer production contributes significantly to greenhouse gas emissions.
Excess fertilizer leads to nutrient runoff, algal blooms, and eutrophication.
Focus on nitrogen deposition:
Human activities contribute to both wet and dry nitrogen deposition.
Organic nitrogen deposition accounts for approximately one-third of total deposition.
Eutrophication process leads to:
Harmful algal blooms.
Fish kills due to dead zones characterized by:
Increased nutrients.
Rapid algal or bacterial growth.
Decreased oxygen levels.
Death of aquatic organisms affected by toxic algal blooms.
Understanding of the eutrophication cascade:
Key steps include increased nutrients, algal growth, oxygen depletion, and subsequent algal decline.
Nutrient inputs and recycling mechanisms:
Chemical weathering of rocks increases available nutrients (P, K, Mg, Ca).
Biological processes contribute to fixed nitrogen in ecosystems.
Atmospheric deposition introduces nutrients via rain, airborne particles, or gases.
Importance of recycling:
Most "active" nutrients in ecosystems are recycled; nutrient resorption is crucial.
Human activities tend to disrupt natural nutrient cycles, increasing both inputs and outputs.
Analysis of nitrogen inputs and outputs:
Inputs include nitrogen fixation facilitated by specific bacteria.
Outputs account for denitrification processes and non-bacteria mediated nitrate leaching.
Key factors influencing soil characteristics:
Climate: affects weathering processes.
Organisms: contribute to soil through biological activity.
Relief: topography influences soil movement and weathering.
Parent material: original composition of the soil.
Time: duration of weathering and plant nutrient utilization plays a significant role.
Influential figure in this context: Hans Jenny (1899-1992).
Research conducted on Hawaiian islands (volcanic origins) aims to evaluate the impact of time on nutrient availability:
Controlled conditions for plant type, slope, and rainfall to study nutrient changes.
Findings indicate an increase in nitrogen over time due to fixation and recycling, while phosphorus initially rises after volcanic eruption but declines due to weathering.
Overview of changes in nutrient types and concentrations:
Dramatic shifts in extractable nutrients, cations, and foliar N & P concentrations.
Figure summaries illustrate variations in plant-available nutrients across different substrate ages.