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Management Impacts on Soil Microbial Nitrogen Cycling
K. Thompson, BSc, PhD
February 12 2019
karenthompson@trentu.ca
@KarenAshleyTee
My Background
• BSc Honours in Environmental Sciences,
UWO (2007)
• Sewoon Foreign Academy and Chosun
University, Gwangju, S. Korea (2007-2009)
• Japan, SE Asia, Russia, England, Costa Rica
(2010)
• PhD at the University of Guelph, in the
School of Environmental Sciences (Land
Resource Sciences) (2016)
• Postdoc at the University of Alberta, in the
faculty of Agriculture, Life and
Environmental Sciences (2016-2017) 2
Current and Upcoming Projects
in the ASH Lab at TrentU
• “Regenerative Agriculture in Action” – Intercropping
Demo Plots (OSCIA) (Matt Porter)
• “Feeding soil with agri-food waste” – Abbey Gardens
partnership (E. Stewart, R. Chan)
• “Insect biodiversity in hedgerows” (D. Beresford, A.
Kasaree)
• “Integrated pest management in greenhouse
floriculture” (D. Beresford, B. Foster)
• “Feasibility of small-scale farming to increase
sustainability in Jamaica” (M. Classens, M. Beerman)
• Impacts of Cropping Systems Management and
Climate Change on Microbial C and N – TBD ☺
What is Sustainable Agriculture?
→Agricultural production
systems that produce food, fuel
and fibre in an ethical,
responsible, and efficient
manner that conserves
biodiversity and the surrounding
environment, produces healthy
food, is profitable for producers,
and promotes valuable
ecosystem goods and services.
4
Need for Efficient Production
Challenges for Sustainable
Agricultural Systems
→Increasing population’s needs for food, fuel,
fibre
→Pest, pathogens
→Changes in land management, LUC
→Reduction in cropping system diversity
→Climate change
6
Systems
Based
Approach
The whole is more than the sum of its parts
Biological
Indicators of
Soil Health
PHYSICAL
Soil Type
Structure and
aeration
Water
infiltration and
retention
CHEMICAL
Available
nutrition
Optimal pH
BIOLOGICAL
Diversity
Nutrient Cycling
Disease /pest
suppression
SOIL HEALTH
How important are these
tiny ‘bugs’ really?
Individuals
Populations
Communities
10
How Diverse are Soil Microbes?
Communities
Soil Communities
12
Soil Microbial Communities Drive GHG Emissions
CO2 N2O CH4
SOIL MICROBIAL COMMUNITY
Nitrification &
Denitrification
Decomposition Methanogenesis
Heterogeneity of soil
Processes co-occurring, spatial and temporal hot
‘spot’s (‘/moments’)
How do we study soil microbial communities?
1. Collect soils
2. Extract nucleic acids
3. Use molecular methods
DNA = “Who’s there”
RNA = “Who’s potentially
active”
Flow of Genetic Info
• DNA = “Who’s there”
• RNA = “Who’s potentially active”
Denitrification and
Nitrification
19
Adapted from:
Snider, D.; Thompson, K.; Wagner-Riddle, C.; Spoelstra, J.
and K. Dunfield (2015). Soil Biology & Biochemistry 88 (2015)
197-213
Images Source: Googe Maps, 2013
Alternate Renewable Fuel Trial
Agricultural Greenhouse Gas Program Trial
20
Perennials Decrease Potential N Losses
nosZ
Annual Rotation
Miscanthus
lognosZgenecopyg
-1
drysoil
5.0
5.2
5.4
5.6
5.8
6.0
21
N2O
Consumption
Thompson, K.A., Deen, B., and K.E. Dunfield. 2016. SOIL 2(4):
523-535
Residue Management Influences SMCs
22
Standing Miscanthus
Before Spring Harvest Residue Return After Spring Harvest in Miscanthus
Plots
Residue Return Increased N2O Mitigation Potential
nosZ cDNA (transcript abundance)
+R -R N
lognosZtranscriptcopypergramdrysoil
2.0
2.2
2.4
2.6
2.8
3.0
3.2
3.4
23
N2O
Consumption
Thompson, K. A., Deen, B. & Dunfield, K. E.
Appl. Soil Ecol. 130, 79–83 (2018).
Project Summary • Miscanthus produces large yields in variable Ontario
climatic conditions.
• Soils under miscanthus supported significantly higher
nosZ gene abundances (larger N2O-reducing
communities) than the traditional land use of corn-
soybean.
24
Soil microbial communities
as potential regulators of in
situ N2O fluxes in annual
and perennial cropping
systems
*Thompson, K. A., Bent, E., Abalos, D.,
Wagner-Riddle, C., and K. E. Dunfield. Soil
Biology and Biochemistry 103 (2016) 262-
273
Context of Study
•Perennial and annual
crops provide varied C
and N inputs
•Liquid dairy manure
(LDM) added to soils
provides C for
denitrification and organic
N and NH4-N that can be
nitrified.
Objective and Research Questions
Are N-cycling microbial community size or structure affected by:
•Perennial vs. annual cropping systems
•LDM management in annual cropping systems
•Ploughing in perennial cropping systems
…and if so do these differences relate to N2O fluxes over time?
Field Comparisons
•Perennial vs. Annual Systems
•LDM application timing in Annual
Systems
•Ploughing in Perennial System
28
Hay ploughed October 2013
Corn: approx. 135 kg N ha-1 liquid dairy manure, November or April,
(Starting Fall 2011)
Hay: approx. 90 kg N ha-1 liquid dairy manure, June (Starting Spring
2012)
=PH
=FMC
=SMC
Methods
• Soil collected along transects in 2012 and 2014.
• DNA extracted from soil
• qPCR used to enumerate nitrifier and denitrifier
gene abundances
• Gene amplicon libraries prepared and amplicons
sequenced (MiSeq), resulting sequences clustered
into OTUs
Gene Targets:
• Denitrifiers = nirS, nirK and nosZ
• Nitrifiers = amoA and crenamoA
Annual vs.
Perennial
Systems
30
2012 2013
MonthlyN2OFlux(kgNha-1)
31
PH FMC SMC PH FMC SMC PH FMC SMC
PH FMC SMC PH FMC SMC PH FMC SMC
Total Bacteria
Denitrifiers
Nitrifiers
= significantly different at p< 0.05
PH = Perennial Hay; FMC= Fall-applied Manure, Corn;
SMC= Spring-applied Manure, Corn
Axis 1 (47.0%)
-1.0 -0.8 -0.6 -0.4 -0.2 0.0 0.2 0.4 0.6 0.8
Axis2(29.5%)
0.0
0.2
0.4
0.6
0.8
1.0
1.2
Axis 1 (68.6%)
-2.0 -1.5 -1.0 -0.5 0.0 0.5 1.0
Axis2(17.9%)
-1.0
-0.8
-0.6
-0.4
-0.2
0.0
0.2
0.4
0.6
nirS nirK
Hay Hay
Spring
Corn
Spring
Corn
Fall
Corn Fall
Corn
Community Profiles as Influenced by Annual vs.
Perennial Cropping Systems
32
p<0.05 p<0.05
LDM Application Timing
33
2012 2013 2014
MonthlyN2OFlux(kgNha-1)
2012 2014
2012 2014 2012 2014
2012 2014
FMC SMC
FMC SMC
FMC SMCFMC SMCFMC SMC
FMC SMCFMC SMCFMC SMC
NitrifiersTotal Bacteria
Denitrifiers
34
PH = Perennial Hay
FMC= Fall-applied Manure, Corn
SMC= Spring-applied Manure, Corn
= significantly different at p< 0.05
Axis 1 (47.0%)
0.1 0.2 0.3 0.4 0.5 0.6 0.7 0.8
Axis2(29.5%)
-1.5
-1.0
-0.5
0.0
0.5
1.0
Axis 1 (68.6%)
-0.6 -0.4 -0.2 0.0 0.2 0.4 0.6 0.8 1.0
Axis2(17.9%)
-1.0
-0.8
-0.6
-0.4
-0.2
0.0
0.2
0.4
0.6
nirK nirS
Community Profiles as Influenced by LDM
Application Timing
35
p<0.05p<0.05
NS
Ploughing in Perennial System
36
PLOUGH
2012 2013 2014
MonthlyN2OFlux(kgNha-1)
Effects of Ploughing
37
2012 2014
Denitrifiers
= significantly different
at p< 0.05
nosZ
Axis 1 (38.7%)
-1.5 -1.0 -0.5 0.0 0.5 1.0 1.5
Axis2(32.4%)
-1.5
-1.0
-0.5
0.0
0.5
1.0
1.5
amoA
Axis 1 (77.9%)
-2.5 -2.0 -1.5 -1.0 -0.5 0.0 0.5 1.0 1.5
Axis2(11.3%)
-1.5
-1.0
-0.5
0.0
0.5
1.0
Axis 1 (68.6%)
-2.0 -1.5 -1.0 -0.5 0.0 0.5 1.0 1.5
Axis2(17.9%)
-1.0
-0.5
0.0
0.5
1.0
1.5
nirK
Axis 1 (47.0%)
-1.5 -1.0 -0.5 0.0 0.5 1.0
Axis2(29.5%) -1.5
-1.0
-0.5
0.0
0.5
1.0
1.5
amoA
nirS nirK
nosZ
Hay
Hay
Hay
Hay
plough
plough
plough
plough
p<0.05
38
Project Conclusions
• Distinct N-cycling communities were associated with land use and
management.
• Shifts in N-cycling microbial communities demonstrated relationships
with agricultural management, which were associated with differences in
N2O flux.
• The size of the N2O-reducing community (nosZ) and specific OTUs may
be largely responsible for N2O production and consumption in soils.
3
9
Molecular Techniques and stable isotope ratios at natural
abundance give complementary inferences about N2O
production pathways in an agricultural soil following a
rainfall event
40
• Snider, D., Thompson, K., Wagner-Riddle, C., Spoelstra, J., Dunfield, K. Soil Biology and Biochemistry (2015) 88, 1–17.
Context of Study
Sampling over a N2O emission event
•Liquid dairy manure (LDM) added to soils provides C for
denitrification and organic N and NH4-N that can be nitrified.
•Large fluxes of N2O often occur following the application of
manure to soil.
•Large N2O emissions are also common after rainfall in soils
affected by drought or extended dry periods.
Objective and
Research
Questions
42
• Use micrometeorological, stable isotope, and
molecular methods to determine the short-
term dynamics of N2O production processes in
soil.
• Do stable isotope and molecular
measurements provide similar inferences
about N2O soil processes occurring over an
emission event?
Significance of Study
This is the first field
study to combine
stable isotope and
molecular methods
to study N2O
production
processes in
manure-amended
soils in situ.
N2O Flux After Rainfall
44
N-Cycling SMCs Increase
45
Significant increase in the size of the N-cycling communities
May 31 June 2 June 8 May 31 June 2 June 8 May 31 June 2 June 8 May 31 June 2 June 8
N2O
Consumption
N2O
Production
Isotopic composition of N2O in the soil
46
Microbial Results Summary
• Molecular analyses revealed abundant and
potentially active nitrifying and denitrifying microbial
communities before and after the rainfall in both fields.
• Following the onset of rain, there was a rapid
response in the soil microbial communities that
stimulated a large flux of N2O via nitrifier-denitrification
and denitrification.
Project Conclusions
•Stable isotopes were useful for directly tracking the
pathways of N2O production.
•Molecular analyses revealed the status of the N
cycling communities before, during and after the
emission event.
•Combined, these methods explained observed
differences in N2O fluxes between fields and gave
complementary results.
Project Background
• Construction of a 500
Kva DC transmission line
in 2014-2015 by ATCO in
SE Alberta provided a
novel research
opportunity to refine
BMPs for transmission
line construction.
Thompson, K., James, K., Najafi, F.,Buckley, S.,
Quideau, S.,Bent, E. Carlyle, C, and E. Bork
(5 manuscripts in prep)
50
Do access mats mitigate the
negative impacts of industrial
traffic?
Disturbance Mitigation
Construction for oil & gas and
powerlines use modern mitigation
tools such as wooden access mats.
• Redistribute weight
• Durable work surface
• Reduce soil rutting & compression
• Prevent ripping of vegetation
• High cost & direct impacts on
vegetation
Study Site
• Mattheis Research Ranch –
Rangeland Research Institute,
University of Alberta
• Mixedgrass prairie
Study Sites
Loamy Soils:
Hesperostipa comata
Koeleria macrantha
Bouteloua gracilis
Pascopyron smitthii
Bouteloua gracilis
Sandy Soils:
Hesperostipa
comata
Carex spps.
Calamovilfa
longifolia
Soil was collected from two grassland sites (RCBD design, one
sandy and one loamy soil) in 2015 and 2016 from natural
vegetation, direct traffic, and traffic overtop of matting.
54
Direct Traffic
Access Mat+
Traffic
Natural
Vegetation
1. Extract – tells us “Who’s there?”
2. Use qPCR to quantify the number of gene ( ) copies
present – tells us “How large is the community?”
3. Use Illumina sequencing to characterize microbial
communities (diversity, community structure)
Traffic Treatments
Impacted Soil
Moisture
→Access mats increased soil
moisture in year 1
→Direct traffic showed
positive legacy effects on soil
moisture in year 2
→Direct traffic increased soil
compaction & bulk density,
and slowed water infiltration
SoilMoisture(g/g)
0
5
10
15
20
25
30
Control
Access Mat
Traffic Only
2015 2016
A
B
BC
CD
D
BC
Disturbance
Altered Soil
Chemistry
AAB
B
AA
B B
→ Direct traffic had higher pH than AM plots.
→Direct traffic (TON) increased soil N and C compared to control
(CON) and access mat (AM) plots.
Soil Texture
Influenced
Total Soil
Bacterial
Community
Size
log16SrRNAgenecopiespergdrysoil
9.0
9.2
9.4
9.6
9.8
10.0
Sandy Soil Loamy Soil
A
B
Traffic and
Access Mats
Influenced
Total Soil
Fungal
Community
Size
2015 2016
A A
B B
→Both disturbances decreased the size of the fungal community in 2015
→ Direct traffic had positive legacy effects on the fungal community in 2016
Disturbance
Variably
Impacted the
Size of the
Nitrifying
Community
CON RM TON
logamoAgenecopiespergdrysoil
5.0
5.2
5.4
5.6
5.8
6.0
6.2
B
AB
A *p=0.0704
Control Access Mat DirectTraffic
→Traffic treatments influenced the size of the nitrifying community that
contributes to N O production.
Traffic Impacts on Fungal Communities
p<0.05
4381 bacterial 16S rRNA OTUs,
1418 ITS OTUs, and 52 archaeal
16S rRNA OTUs
Fungal community profiles were
significantly different between
AM and TON plots in both years
of sampling.
AM
CON
TON
Indicator Species Analysis
• 43 Bacterial OTUs
• 26 Fungal OTUs
• 6 Archaeal OTUs
CON: associated with aerobic bacterial species and C-cycling and N2-
fixing OTUs.
TON: associated with anaerobic species including Cyanobacteria spp. And
Gemmata spp.
AM: associated with a number of potential fungal plant pathogens
Conclusions
AM placed on actively growing vegetation for
12 weeks in the spring had a large impact on
soil microbial communities, particularly fungi.
The use of AM should not be undertaken
without consideration of soil texture and
amount of traffic prairie will be exposed to.
AM did not sufficiently mitigate impacts of
industrial traffic on soil microbial communities
– however, this study utilized a limited number
of traffic passes.
Impacts of in situ Tower Construction
Project Summary
Fungal communities and some N-cycling
microbial groups responded to the type of
traffic disturbance and tower construction
methods, suggesting different construction
techniques may alter soil C storage, and the
potential of the microbial community to
produce and consume N2O, therefore
influencing associated ecosystem
functioning during grassland recovery.
Current Work Underway is Addressing the Role of AMP
(adaptive, multi-paddock) Grazing on soil C, microbial
communities, plant communities, and GHGs
65
Summary
• Soil microbial communities are
influenced by our
management choices
• Interdisciplinary, systems-
based approaches are required
• Successful production relies on
management of soil microbial
communities that promote
crop productivity and efficient
input use
Future Research
Linking changes in soil microbial
communities with agricultural management
within specific:
•Climates
•Geographies
•Soil types
•To determine the fate of C and N in soil
•To create BMPs to decrease N losses, build
soil C, maintain or promote EGS from our
agro-ecosystems.
67

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Management Impacts on Soil Microbial Nitrogen Cycling

  • 1. Management Impacts on Soil Microbial Nitrogen Cycling K. Thompson, BSc, PhD February 12 2019 karenthompson@trentu.ca @KarenAshleyTee
  • 2. My Background • BSc Honours in Environmental Sciences, UWO (2007) • Sewoon Foreign Academy and Chosun University, Gwangju, S. Korea (2007-2009) • Japan, SE Asia, Russia, England, Costa Rica (2010) • PhD at the University of Guelph, in the School of Environmental Sciences (Land Resource Sciences) (2016) • Postdoc at the University of Alberta, in the faculty of Agriculture, Life and Environmental Sciences (2016-2017) 2
  • 3. Current and Upcoming Projects in the ASH Lab at TrentU • “Regenerative Agriculture in Action” – Intercropping Demo Plots (OSCIA) (Matt Porter) • “Feeding soil with agri-food waste” – Abbey Gardens partnership (E. Stewart, R. Chan) • “Insect biodiversity in hedgerows” (D. Beresford, A. Kasaree) • “Integrated pest management in greenhouse floriculture” (D. Beresford, B. Foster) • “Feasibility of small-scale farming to increase sustainability in Jamaica” (M. Classens, M. Beerman) • Impacts of Cropping Systems Management and Climate Change on Microbial C and N – TBD ☺
  • 4. What is Sustainable Agriculture? →Agricultural production systems that produce food, fuel and fibre in an ethical, responsible, and efficient manner that conserves biodiversity and the surrounding environment, produces healthy food, is profitable for producers, and promotes valuable ecosystem goods and services. 4
  • 5. Need for Efficient Production
  • 6. Challenges for Sustainable Agricultural Systems →Increasing population’s needs for food, fuel, fibre →Pest, pathogens →Changes in land management, LUC →Reduction in cropping system diversity →Climate change 6
  • 7. Systems Based Approach The whole is more than the sum of its parts
  • 8. Biological Indicators of Soil Health PHYSICAL Soil Type Structure and aeration Water infiltration and retention CHEMICAL Available nutrition Optimal pH BIOLOGICAL Diversity Nutrient Cycling Disease /pest suppression SOIL HEALTH
  • 9. How important are these tiny ‘bugs’ really?
  • 12. 12
  • 13.
  • 14.
  • 15. Soil Microbial Communities Drive GHG Emissions CO2 N2O CH4 SOIL MICROBIAL COMMUNITY Nitrification & Denitrification Decomposition Methanogenesis
  • 16. Heterogeneity of soil Processes co-occurring, spatial and temporal hot ‘spot’s (‘/moments’)
  • 17. How do we study soil microbial communities? 1. Collect soils 2. Extract nucleic acids 3. Use molecular methods DNA = “Who’s there” RNA = “Who’s potentially active”
  • 18. Flow of Genetic Info • DNA = “Who’s there” • RNA = “Who’s potentially active”
  • 19. Denitrification and Nitrification 19 Adapted from: Snider, D.; Thompson, K.; Wagner-Riddle, C.; Spoelstra, J. and K. Dunfield (2015). Soil Biology & Biochemistry 88 (2015) 197-213
  • 20. Images Source: Googe Maps, 2013 Alternate Renewable Fuel Trial Agricultural Greenhouse Gas Program Trial 20
  • 21. Perennials Decrease Potential N Losses nosZ Annual Rotation Miscanthus lognosZgenecopyg -1 drysoil 5.0 5.2 5.4 5.6 5.8 6.0 21 N2O Consumption Thompson, K.A., Deen, B., and K.E. Dunfield. 2016. SOIL 2(4): 523-535
  • 22. Residue Management Influences SMCs 22 Standing Miscanthus Before Spring Harvest Residue Return After Spring Harvest in Miscanthus Plots
  • 23. Residue Return Increased N2O Mitigation Potential nosZ cDNA (transcript abundance) +R -R N lognosZtranscriptcopypergramdrysoil 2.0 2.2 2.4 2.6 2.8 3.0 3.2 3.4 23 N2O Consumption Thompson, K. A., Deen, B. & Dunfield, K. E. Appl. Soil Ecol. 130, 79–83 (2018).
  • 24. Project Summary • Miscanthus produces large yields in variable Ontario climatic conditions. • Soils under miscanthus supported significantly higher nosZ gene abundances (larger N2O-reducing communities) than the traditional land use of corn- soybean. 24
  • 25. Soil microbial communities as potential regulators of in situ N2O fluxes in annual and perennial cropping systems *Thompson, K. A., Bent, E., Abalos, D., Wagner-Riddle, C., and K. E. Dunfield. Soil Biology and Biochemistry 103 (2016) 262- 273
  • 26. Context of Study •Perennial and annual crops provide varied C and N inputs •Liquid dairy manure (LDM) added to soils provides C for denitrification and organic N and NH4-N that can be nitrified.
  • 27. Objective and Research Questions Are N-cycling microbial community size or structure affected by: •Perennial vs. annual cropping systems •LDM management in annual cropping systems •Ploughing in perennial cropping systems …and if so do these differences relate to N2O fluxes over time?
  • 28. Field Comparisons •Perennial vs. Annual Systems •LDM application timing in Annual Systems •Ploughing in Perennial System 28 Hay ploughed October 2013 Corn: approx. 135 kg N ha-1 liquid dairy manure, November or April, (Starting Fall 2011) Hay: approx. 90 kg N ha-1 liquid dairy manure, June (Starting Spring 2012) =PH =FMC =SMC
  • 29. Methods • Soil collected along transects in 2012 and 2014. • DNA extracted from soil • qPCR used to enumerate nitrifier and denitrifier gene abundances • Gene amplicon libraries prepared and amplicons sequenced (MiSeq), resulting sequences clustered into OTUs Gene Targets: • Denitrifiers = nirS, nirK and nosZ • Nitrifiers = amoA and crenamoA
  • 31. 31 PH FMC SMC PH FMC SMC PH FMC SMC PH FMC SMC PH FMC SMC PH FMC SMC Total Bacteria Denitrifiers Nitrifiers = significantly different at p< 0.05 PH = Perennial Hay; FMC= Fall-applied Manure, Corn; SMC= Spring-applied Manure, Corn
  • 32. Axis 1 (47.0%) -1.0 -0.8 -0.6 -0.4 -0.2 0.0 0.2 0.4 0.6 0.8 Axis2(29.5%) 0.0 0.2 0.4 0.6 0.8 1.0 1.2 Axis 1 (68.6%) -2.0 -1.5 -1.0 -0.5 0.0 0.5 1.0 Axis2(17.9%) -1.0 -0.8 -0.6 -0.4 -0.2 0.0 0.2 0.4 0.6 nirS nirK Hay Hay Spring Corn Spring Corn Fall Corn Fall Corn Community Profiles as Influenced by Annual vs. Perennial Cropping Systems 32 p<0.05 p<0.05
  • 33. LDM Application Timing 33 2012 2013 2014 MonthlyN2OFlux(kgNha-1)
  • 34. 2012 2014 2012 2014 2012 2014 2012 2014 FMC SMC FMC SMC FMC SMCFMC SMCFMC SMC FMC SMCFMC SMCFMC SMC NitrifiersTotal Bacteria Denitrifiers 34 PH = Perennial Hay FMC= Fall-applied Manure, Corn SMC= Spring-applied Manure, Corn = significantly different at p< 0.05
  • 35. Axis 1 (47.0%) 0.1 0.2 0.3 0.4 0.5 0.6 0.7 0.8 Axis2(29.5%) -1.5 -1.0 -0.5 0.0 0.5 1.0 Axis 1 (68.6%) -0.6 -0.4 -0.2 0.0 0.2 0.4 0.6 0.8 1.0 Axis2(17.9%) -1.0 -0.8 -0.6 -0.4 -0.2 0.0 0.2 0.4 0.6 nirK nirS Community Profiles as Influenced by LDM Application Timing 35 p<0.05p<0.05 NS
  • 36. Ploughing in Perennial System 36 PLOUGH 2012 2013 2014 MonthlyN2OFlux(kgNha-1)
  • 37. Effects of Ploughing 37 2012 2014 Denitrifiers = significantly different at p< 0.05
  • 38. nosZ Axis 1 (38.7%) -1.5 -1.0 -0.5 0.0 0.5 1.0 1.5 Axis2(32.4%) -1.5 -1.0 -0.5 0.0 0.5 1.0 1.5 amoA Axis 1 (77.9%) -2.5 -2.0 -1.5 -1.0 -0.5 0.0 0.5 1.0 1.5 Axis2(11.3%) -1.5 -1.0 -0.5 0.0 0.5 1.0 Axis 1 (68.6%) -2.0 -1.5 -1.0 -0.5 0.0 0.5 1.0 1.5 Axis2(17.9%) -1.0 -0.5 0.0 0.5 1.0 1.5 nirK Axis 1 (47.0%) -1.5 -1.0 -0.5 0.0 0.5 1.0 Axis2(29.5%) -1.5 -1.0 -0.5 0.0 0.5 1.0 1.5 amoA nirS nirK nosZ Hay Hay Hay Hay plough plough plough plough p<0.05 38
  • 39. Project Conclusions • Distinct N-cycling communities were associated with land use and management. • Shifts in N-cycling microbial communities demonstrated relationships with agricultural management, which were associated with differences in N2O flux. • The size of the N2O-reducing community (nosZ) and specific OTUs may be largely responsible for N2O production and consumption in soils. 3 9
  • 40. Molecular Techniques and stable isotope ratios at natural abundance give complementary inferences about N2O production pathways in an agricultural soil following a rainfall event 40 • Snider, D., Thompson, K., Wagner-Riddle, C., Spoelstra, J., Dunfield, K. Soil Biology and Biochemistry (2015) 88, 1–17.
  • 41. Context of Study Sampling over a N2O emission event •Liquid dairy manure (LDM) added to soils provides C for denitrification and organic N and NH4-N that can be nitrified. •Large fluxes of N2O often occur following the application of manure to soil. •Large N2O emissions are also common after rainfall in soils affected by drought or extended dry periods.
  • 42. Objective and Research Questions 42 • Use micrometeorological, stable isotope, and molecular methods to determine the short- term dynamics of N2O production processes in soil. • Do stable isotope and molecular measurements provide similar inferences about N2O soil processes occurring over an emission event?
  • 43. Significance of Study This is the first field study to combine stable isotope and molecular methods to study N2O production processes in manure-amended soils in situ.
  • 44. N2O Flux After Rainfall 44
  • 45. N-Cycling SMCs Increase 45 Significant increase in the size of the N-cycling communities May 31 June 2 June 8 May 31 June 2 June 8 May 31 June 2 June 8 May 31 June 2 June 8 N2O Consumption N2O Production
  • 46. Isotopic composition of N2O in the soil 46
  • 47. Microbial Results Summary • Molecular analyses revealed abundant and potentially active nitrifying and denitrifying microbial communities before and after the rainfall in both fields. • Following the onset of rain, there was a rapid response in the soil microbial communities that stimulated a large flux of N2O via nitrifier-denitrification and denitrification.
  • 48. Project Conclusions •Stable isotopes were useful for directly tracking the pathways of N2O production. •Molecular analyses revealed the status of the N cycling communities before, during and after the emission event. •Combined, these methods explained observed differences in N2O fluxes between fields and gave complementary results.
  • 49. Project Background • Construction of a 500 Kva DC transmission line in 2014-2015 by ATCO in SE Alberta provided a novel research opportunity to refine BMPs for transmission line construction. Thompson, K., James, K., Najafi, F.,Buckley, S., Quideau, S.,Bent, E. Carlyle, C, and E. Bork (5 manuscripts in prep)
  • 50. 50 Do access mats mitigate the negative impacts of industrial traffic?
  • 51. Disturbance Mitigation Construction for oil & gas and powerlines use modern mitigation tools such as wooden access mats. • Redistribute weight • Durable work surface • Reduce soil rutting & compression • Prevent ripping of vegetation • High cost & direct impacts on vegetation
  • 52. Study Site • Mattheis Research Ranch – Rangeland Research Institute, University of Alberta • Mixedgrass prairie
  • 53. Study Sites Loamy Soils: Hesperostipa comata Koeleria macrantha Bouteloua gracilis Pascopyron smitthii Bouteloua gracilis Sandy Soils: Hesperostipa comata Carex spps. Calamovilfa longifolia
  • 54. Soil was collected from two grassland sites (RCBD design, one sandy and one loamy soil) in 2015 and 2016 from natural vegetation, direct traffic, and traffic overtop of matting. 54 Direct Traffic Access Mat+ Traffic Natural Vegetation 1. Extract – tells us “Who’s there?” 2. Use qPCR to quantify the number of gene ( ) copies present – tells us “How large is the community?” 3. Use Illumina sequencing to characterize microbial communities (diversity, community structure)
  • 55. Traffic Treatments Impacted Soil Moisture →Access mats increased soil moisture in year 1 →Direct traffic showed positive legacy effects on soil moisture in year 2 →Direct traffic increased soil compaction & bulk density, and slowed water infiltration SoilMoisture(g/g) 0 5 10 15 20 25 30 Control Access Mat Traffic Only 2015 2016 A B BC CD D BC
  • 56. Disturbance Altered Soil Chemistry AAB B AA B B → Direct traffic had higher pH than AM plots. →Direct traffic (TON) increased soil N and C compared to control (CON) and access mat (AM) plots.
  • 58. Traffic and Access Mats Influenced Total Soil Fungal Community Size 2015 2016 A A B B →Both disturbances decreased the size of the fungal community in 2015 → Direct traffic had positive legacy effects on the fungal community in 2016
  • 59. Disturbance Variably Impacted the Size of the Nitrifying Community CON RM TON logamoAgenecopiespergdrysoil 5.0 5.2 5.4 5.6 5.8 6.0 6.2 B AB A *p=0.0704 Control Access Mat DirectTraffic →Traffic treatments influenced the size of the nitrifying community that contributes to N O production.
  • 60. Traffic Impacts on Fungal Communities p<0.05 4381 bacterial 16S rRNA OTUs, 1418 ITS OTUs, and 52 archaeal 16S rRNA OTUs Fungal community profiles were significantly different between AM and TON plots in both years of sampling. AM CON TON
  • 61. Indicator Species Analysis • 43 Bacterial OTUs • 26 Fungal OTUs • 6 Archaeal OTUs CON: associated with aerobic bacterial species and C-cycling and N2- fixing OTUs. TON: associated with anaerobic species including Cyanobacteria spp. And Gemmata spp. AM: associated with a number of potential fungal plant pathogens
  • 62. Conclusions AM placed on actively growing vegetation for 12 weeks in the spring had a large impact on soil microbial communities, particularly fungi. The use of AM should not be undertaken without consideration of soil texture and amount of traffic prairie will be exposed to. AM did not sufficiently mitigate impacts of industrial traffic on soil microbial communities – however, this study utilized a limited number of traffic passes.
  • 63. Impacts of in situ Tower Construction
  • 64. Project Summary Fungal communities and some N-cycling microbial groups responded to the type of traffic disturbance and tower construction methods, suggesting different construction techniques may alter soil C storage, and the potential of the microbial community to produce and consume N2O, therefore influencing associated ecosystem functioning during grassland recovery.
  • 65. Current Work Underway is Addressing the Role of AMP (adaptive, multi-paddock) Grazing on soil C, microbial communities, plant communities, and GHGs 65
  • 66. Summary • Soil microbial communities are influenced by our management choices • Interdisciplinary, systems- based approaches are required • Successful production relies on management of soil microbial communities that promote crop productivity and efficient input use
  • 67. Future Research Linking changes in soil microbial communities with agricultural management within specific: •Climates •Geographies •Soil types •To determine the fate of C and N in soil •To create BMPs to decrease N losses, build soil C, maintain or promote EGS from our agro-ecosystems. 67