Post on 14-Feb-2022
Nutrient dynamics in
freshwaters
Chapter 13 (C)
Chapter 14 (N, P)
The greatest analgesic, soporific, stimulant, tranquilizer, narcotic, and to some extent
even antibiotic -- in short, the closest thing to a genuine panacea -- known to medical
science is work. -Thomas Szasz, author, professor of psychiatry (b. 1920)
Today
Nutrients dynamics
Lab: move up the OM collection
Test 3 (Wed)
Next week
– Hydrology
– Lab: flow regime analysis
– EOW 17-18
Nutrient cycle: Terms
Flux vs. Compartments (source/sink)
Budget
Assimilation
Re-mineralization
Sequestration
Redox
– High (oxic)
– Low (reducing, e.g., methanogenesis CO2
CH4)
FIGURE 13.7
Diagram of a hypothetical nutrient cycle. This will be the general format used to represent nutrient cycles. Oxic
processes are above the center line and anoxic processes are below. Those that move on the center line are required,
independent of O2 concentration. Inorganic forms are listed from left to right, from reduced to oxidized. Thus,
transformations are generally occurring with potential energy if they move from left to right in the top half of the
diagram or from right to left in the bottom half of the diagram.
Generalized Nutrient Cycle
Carbon
Why do you need it?
Carbon Cycle
Compartments
– Sources
– Sinks (sequestered C)
Fluxes (i.e., processes)
– Assimilatory
– Re-mineralization
Budgets (ignore for now)
©2010 Elsevier, Inc.
FIGURE 13.8
A diagram of the generalized carbon cycle.
Nitrogen
Why?
Forms of N
N2
N2O
Nitrate (NO3-)*
Nitrite (NO2-)
Ammonium (NH4-)*
NH3
DIN (sum of the ions)
DON (0.45 µm filter)
PON (e.g., fish)
N sources/sinks
N processes
N fixation
– Lightning
– Rhizobia
– Haber process
– Burning fossil fuels
– Cyanobacteria
Heterocytes and nitrogenase
©2010 Elsevier, Inc.
FIGURE 14.1
Streamers composed of the sulfur-oxidizing bacterium Thermothrix at Mammoth Terrace, Yellowstone National
Park (courtesy of R. W. Castenholz) and a transmission electron micrograph of a heterocyst (the site of nitrogen
fixation in Nostoc and other cyanobacteria) attached to a smaller dividing vegetative cell with a diameter of
approximately 8 μm. (Micrograph courtesy of N. J. Lang).
N processes
Nitrification
Denitification
– Nitrate reduction
N processes
Uptake
Excretion
Ammonification
N Cycle
N2
N fixation (anaerobic, cyanobacteria) PON
Detrital
PoolDie
PON
Animals
DON
NH4-
DON
NO2-
DON
NO3-
PON
Plants
NO3-
PON
Detrital
Pool
PON
Detrital
Pool
PON
Detrital
Pool
Nitri
fication (
aero
bic
)
Excrete
BGA
PON
Die
©2010 Elsevier, Inc.
FIGURE 14.6
A conceptual diagram of the nitrogen cycle.
Nitrogen Dynamics
Sources
– Lakes
– Streams
Sinks/Losses
– Lakes
– Streams
Seasonal N Distribution in Lakes
Nitra
te, N
itriteN
itriteN
H4
Seasonal N Distribution in Lakes
FIGURE 14.4
Distribution of nitrate (A) and ammonium (B) in hypereutrophic Wintergreen Lake, Michigan, as a function of depth
and time. Ice cover occurred from January to March. Darker colors represent higher concentrations. Contours are
reported in μg liter21. (Reproduced with permission from Wetzel, 1983).
N in Streams
©2010 Elsevier, Inc.
FIGURE 14.7
Correlation between nitrate intake and rates of gastrointestinal cancer. (After P. E. Hartman. 1983. Reprinted by
permission of Wiley–Liss, Inc., a subsidiary of John Wiley & Sons, Inc.).
Phosphorus
Why needed?
Forms of P
Rare
Soluble Particulate
Inorganic PO43- (BAP) Mineral apatites
Organic ATP, phospholipids Detritus, POP
Ca(PO4)2
FePO4
e.g., a fish
Phosphorus fluxes
Geophysical weathering
Cycling (rapid uptake)
– DOP
– POP
– DIP
Sedimentation (attachment)
– Importance of macrophytes
Role of P-ase (alkaline phosphatase)
©2010 Elsevier, Inc.
FIGURE 14.9
A diagram of the phosphorus cycle.
P Cycle in a Lake
Rock
Inorganic
sediments
DIP,
BAP
Organic
sediments
Trophic
dynamics
Decay
Organic detritus,
soluble POP,
leaching, lysis
Total P distribution
90% particulate
10% soluble
P – Sediment Interaction
Mechanical attachment of P
P dynamics
Sources
– Lakes
– Streams
Sinks/Losses
– Lakes
– Streams
What is more N and P limited?
Streams or lakes? Why?
Nutrient Spiraling
Time for
1 cycleSpiral distance
Nutrient
available
here
©2010 Elsevier, Inc.
FIGURE 24.7
A diagram of nutrient spiraling in streams. S is the total spiral length, Sp is the time spent in particulate form in
water column or the benthic zone and Sw is the average time spent in the water. Average velocity is greater in the
riffle on the left, so spiral length is greater than in the pool at the right.
Nutrient loading and
Eutrophication
Nutrient loading
N sources (tera grams per year)
N fixation
Lightning – 10
Soil microbes –130
BGA – trivial
Human fertilizers – 80
N fixing crops – 40
Fossil fuels – 20
Deforestation – 40
P sources
Very rare
Human sources (mostly non-point)
– Fertilizers
– Detergents
– Sewage
– Livestock waste
Eutrophication
Human activities
N and P loading
Alteration of physico-chemical
and biological conditions
Processes/Events
Lake Trophic Status
Oligotrophic
Mesotrophic
Eutrophic
Eutrophication
Where is it more of a problem?
– Lakes
– Streams / rivers
Mitigation
Remove cause / control inputs
– Point sources
– Non-point
Treat symptoms
– Bio-manipulation
IndicatorsTable 18.1
Chl a indicator
Fig. 18.2
SolutionsHodgson 2005
Dec spiraling distance in
upstream areas and HWs.
Maintain HW structure and
function (retentiveness)
Table 18.3
Trophic cascade theory
FIGURE 12.13
O2 increase
Super-saturation
Anoxia:
Winter kill
Summer kill
Implications for
wetland plants
©2010 Elsevier, Inc.
FIGURE 14.8
A conceptual diagram of the sulfur cycle. A 5 assimilation.
©2010 Elsevier, Inc.
FIGURE 14.10
Concentration of silica as a function of depth and time in hypereutrophic Wintergreen Lake, Michigan (A), and
oligotrophic Lawrence Lake, Michigan (B). Concentrations are given in mg liter21, with darker contour fills
corresponding to greater concentrations. (Reproduced with permission from Wetzel, 1983).
©2010 Elsevier, Inc.
FIGURE 14.11
The relationship between epilimnetic silicon and biomass of the diatom, Asterionella, in Lake Windermere, England.
Note how decreases in dissolved silica correspond with high densities of diatoms. (Data from Lund, 1964).
©2010 Elsevier, Inc.
FIGURE 14.12
A conceptual diagram of the iron cycle.
©2010 Elsevier, Inc.
FIGURE 14.13
Relationship among redox gradients, dissolved oxygen, nutrient concentrations, and functional groups of
microorganisms responsible for biogeochemical fluxes. This figure illustrates the steep gradients that occur at
oxic/anoxic interfaces, and how such interfaces are a hot spot for biogeochemical activities.