Thomas Andrew Black
Relevant Degree Programs
Measurement of greenhouse gas fluxes in agricultural systems
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Graduate Student Supervision
Doctoral Student Supervision
Dissertations completed in 2010 or later are listed below. Please note that there is a 6-12 month delay to add the latest dissertations.
There is a lack of knowledge of the processes controlling the net ecosystem production (NEP) of forest stands after disturbance (e.g., logging and nitrogen (N) fertilization) in the Pacific Northwest. To answer these questions, long-term eddy-covariance (EC) measurements of carbon-dioxide (CO₂) above a Douglas-fir stand on Vancouver Island, Canada were used in this study. Additionally, answering these questions also requires that NEP can be accurately partitioned into gross primary production (GPP) and ecosystem respiration (Re) to understand the biophysical controls of their C dynamics. Therefore, an intensive stable C isotope campaign was conducted and various partitioning techniques were deployed in this study. The Physiological Principles Predicting Growth (3-PG) model was modified to compare its predictions with EC-measured data to better understand the effects of N fertilization on CO₂ and water vapour fluxes. Application of N fertilizer to this stand led to a short-term (first two years) increase in GPP followed by little change over the long term. Re increased over the short-term (first year), while it was appreciably suppressed over the long term. N fertilization resulted in an average increase in NEP by 170 g C m-² year-¹ on average and led to an average increase in annual water use of 15%. The light-inhibition effect of daily Re for the stand during the peak growing season was estimated to be 37% by comparing the nighttime relationship and the stable C isotope methods. The daytime intercept partitioning method only partly accounted for light inhibition effects. By applying four gap-filling models using different partitioning techniques (nighttime relationship, daytime intercept, ANN–nighttime, and FVS–ANN models) on the 18-years of measured data, it was estimated that the mean annual NEP totals ranged from 195 to 238 g C m-² year-¹, hence the choice of the gap-filling model would have a great impact on long-term C budgets. There were even larger differences in Re and GPP estimates. Our findings have implications for the interpretation of EC measurements, a widely-used data source for understanding terrestrial C cycling. I further argue that the consideration of light inhibition of daytime Re in terrestrial ecosystem models is critical.
Plastic film soil mulches (i.e., protective soil covers) and plastic covered low tunnels (i.e., enclosure) have the potential to alter crop microclimate, lengthen the growing-season, and increase plant productivity. A plastic film’s ability to alter microclimate is related to its shortwave (S) and longwave (L) radiative properties (reflectivity (ρ), transmissivity (τ) and absorptivity (α)). This thesis examines the effect of plastic films with different radiative properties on 1) surface energy balance, 2) crop microclimate, and 3) crop productivity.A study of nine plastic film mulches with various radiative properties (Chapter 2) showed that all films increased daily soil heat flux density, including a high ρs value film (0.45), due to its insulating effect at night. A comparison of three black plastic films with high shortwave absorptivity (αs ≈ 0.95) but different αL values showed that low and high αL value films achieved the highest and lowest daytime soil temperatures, respectively.A study of vegetation-free plastic film low tunnels with similar τs but different αL values (Chapter 3) showed that a high αL value cover (i.e., glass-like) increased net longwave radiation inside the low tunnel compared to a low αL value cover, and increased inside air temperature (Tain) by 5 and 2°C during the daytime and nighttime, respectively. A model to predict daytime and nighttime Tain is presented and validated. A study of Padrón peppers (Capsicum annuum) grown inside and outside low tunnels (Chapter 4) showed that low tunnels increase pepper growth, productivity (10%) and growing-season length (~2 weeks), but CO₂ depletion and high water vapour density occurs when leaf area index is high. A study of summer squash (Cucurbita pepo) grown within black plastic mulch showed that the addition of a perforated low tunnel increased yield 27%. A study of broccoli (Brassica oleracea) showed that low tunnels increased yield due to wind protection in spring, which conserved soil moisture and increased Tain during low temperatures. This thesis shows that plastic film covered low tunnels and soil mulches are an effective tool for altering crop microclimate and increasing yield, but trade-offs regarding microclimate exist that crop producers should consider.
Nearly one tenth of the world’s forest is located in Canada, with one third being boreal forest. Understanding how this biome is responding to climate change is important to global carbon (C) and water balances. Long-term climate and eddy-covariance (EC) measurements of C and water vapour fluxes were made on a mature deciduous aspen stand (old aspen, OA) and a mature coniferous black spruce stand (old black spruce, OBS) to determine the impact of climate variations and disturbances on the C and water fluxes, and test if commonly utilized models can successfully model these fluxes. The impact of a defoliation event at OA in the summer of 2016, due to forest tent caterpillar infestation, was investigated and annual GEP was found to be reduced by ~20% that year, leading to the most negative annual NEP (-72 g C m⁻² year⁻¹) over the observation period. Long-term trends in annual climate variables, along with trends in gross ecosystem production (GEP), ecosystem respiration (Re), net ecosystem production (NEP), evapotranspiration (E), P – E, and water use efficiency (WUE = GEP/E) were investigated using 22 and 19 years of continuous data at OA and OBS, respectively. The impacts of growing season (GS) metrics on GS and annual NEP, GEP and E were investigated. Trends were also investigated at GS and monthly scales for climate variables and E, along with the impact of GS metrics on E at GS scale. The two stands showed varied responses to climatic variability, including responses to a multi-year drought that affected both sites but had a larger impact on the C and water fluxes at OA than OBS. The dependence of the canopy conductance (Gc) and E on their controlling variables was investigated at GS and monthly scales for both sites. The Jarvis-Stewart (JS) and modified Ball-Woodrow-Berry (MBWB) models were tested to estimate half-hourly Gc at each site and compute both Gc and E at seasonal to annual scales. This thesis demonstrates the importance of long-term observations in capturing variations in climate and disturbances forests experience, that need to be further studied and modelled for improved understanding of their impacts.
The most recent mountain pine beetle (MPB) (Dendroctonus ponderosae) outbreak in British Columbia (BC), which began in the late 1990s, killed ~54% of the mature merchantable lodgepole pine volume and was expected to impact gross primary productivity (GPP), ecosystem respiration (R) and thus net ecosystem productivity (NEP), as well as evapotranspiration (E), snow accumulation and melt in infested stands due to tree mortality. To quantify these effects, eddy-covariance (EC) measurements of carbon (C) and water vapour fluxes have been made above two not-salvage-harvested MPB-attacked pine stands, one with little understory (MPB-06) and another with considerable understory for ten and six years, respectively, and for three years in a partial-salvage-harvested stand, complemented with short-term EC measurements in nearby clearcuts. To determine long-term recovery of the C and water balances following attack, I modified the 3-PG (Physiological Principles Predicting Growth) model to simulate the effects of MPB attack on MPB-06. Modifications included a 2-layer canopy with a partly-dying overstory and growing understory, water availability from snowmelt, and a heterotrophic respiration sub-model. Modelled monthly and annual fluxes at MPB-06 agreed well with the respective EC-estimated values during the decade following attack. Modelled annual GPP, R, NEP and E decreased by about 52%, 35%, 126% and 62%, respectively, in the first year following attack compared to pre-attack values in 2005. While modelled GPP and R, as well as EC-estimated GPP, showed a relatively steady increase over the following decade, EC-estimated R changed little in the first eight years after attack and then increased in the last two years. Both modelled and measured NEP increased significantly over the decade with MPB-06 becoming C neutral within three to four years following attack. EC-measured annual E remained remarkably stable for five years after the attack, and then increased in the last five years, whereas the model indicated a relatively steady increase over the decade. Model projections for five climate change scenarios show 2026 average GPP, R, NEP and E being 14%, 1%, 65% and 5%, respectively, lower than pre-attack values. The quick recovery suggests that not-salvage-harvesting can be a beneficial management practice for C sequestration and hydrology.
Over the past decade British Columbia (BC) has experienced the largest mountain pine beetle (MPB) outbreak on record. This study used the eddy covariance (EC) technique to examine the impact of the MPB outbreak on the net ecosystem production (NEP) and evapotranspiration (E) of two lodgepole pine stands in the central interior of BC from 2007 to 2010. MPB-06, an 85-year-old stand, and MPB-03, a 110-year-old stand, were first attacked by the beetle in 2006 and 2003, respectively. EC measurements were also made in two harvested stands, one in 2005 and one in 1997 (CC-05 and CC-97, respectively) during the 2007 growing season. Annual NEP increased from -81 to 64 g carbon (C) m-² from 2007 to 2010 at MPB-06 due to an increase in gross ecosystem photosynthesis (Pg). At MPB-03, annual NEP also varied with Pg, ranging from -57 g C m-² in 2007 to 6 g C m-² in 2009. Annual ecosystem respiration (Re) did not vary greatly over the four years at both sites. At MPB-03, Pg was reduced by drought in 2009 and 2010. The increase in Pg at both sites was due to an increase in the photosynthetic capacity of the surviving trees and vegetation, as shown by foliar net-assimilation measurements. Light response analysis indicated that daytime Re values derived using nighttime NEP data were likely realistic estimates of the actual respiratory fluxes. NEP measurements at CC-97 and CC-05, showed that these stands are likely to remain C sources for as many as 10 years following harvesting. There was little interannual variation in E at both sites as the surviving trees and vegetation compensated for reductions in E due to the death of the overstory. Root-zone drainage was much greater at MPB-03 than at MPB-06, due to larger P at MPB-03. Growing season water deficit showed both stands to be water limited in spite of the high proportion of dead pine trees. Results from this study showed the importance of the remaining healthy trees and vegetation in the recovery of these stands from MPB attack.
Master's Student Supervision
Theses completed in 2010 or later are listed below. Please note that there is a 6-12 month delay to add the latest theses.
The three main biogenic greenhouse gases (GHGs), nitrous oxide (N₂O), methane (CH₄) and carbon dioxide (CO₂), are associated with agricultural production and strongly affected by environmental factors, which makes mitigation of GHG emissions a more challenging task in intensive agricultural system in the context of global climate change. Quantification of GHG emissions is of great interest in agroecosystems to better understand flux exchange between agroecosystems and the atmosphere and to provide knowledge for climate change related policy making. However, in Canada, these studies are largely limited to Ontario and the Canadian Prairie provinces, and GHG emissions in the main cropping systems in British Columbia have scarcely been studied. Therefore, this study is aimed at making continuous measurements of N₂O, CO₂ and CH₄ from potato and pea crops in the lower Fraser Valley using the eddy covariance (EC) technique. Furthermore, to cope with the issue of slight spatial inhomogeneity at this study site, flux footprint analysis was used, coupled with EC and closed-chamber measurements. I found that flux footprint correction had the largest effect on N₂O flux compared with CO₂ flux because of more pronounced difference of N₂O flux between two different land surfaces (crop and edge areas). After flux footprint correction, the potato and pea crops were both weak CO₂ sinks with annual net ecosystem exchange values being -57 and -97 g C m⁻² yr⁻¹, respectively. After taking carbon (C) export via crop harvest into account, the potato crop shifted from being a C sink to a C source of 375 g C m⁻² yr⁻¹, while the pea crop became near neutral sequestering only 19 g C m⁻² yr⁻¹. Annual GHG budget was quantified by converting N₂O and CH₄ to CO₂ equivalents using global warming potential on a 100-year timescale, which is 298 for N₂O and 34 for CH₄. The annual GHG budgets were 481 and 200 g CO₂e m⁻² yr⁻¹ for the potato and pea crops respectively. For both potato and pea crops, N₂O contributed the largest proportion to annual total CO₂e and outweighed the CO₂ uptake from the atmosphere, making both crop fields net sources of GHGs.
Unprecedented expansion of unconventional energy resource development has caused concerns about fugitive gas emissions, the patterns of which are not well understood. This study was conducted in north-eastern British Columbia, which is a region of active petroleum resource development, and there is evidence of gas migration at gas wells. A controlled gas injection experiment was conducted at the Hudson’s Hope Field Research Station (HHFRS) near Hudson’s Hope, where 1.5 m³ of synthetic natural gas was injected daily for a period of 66 days, 26 m below the ground (below the water table). The eddy covariance (EC) technique was used to monitor emissions into the atmosphere resulting from the controlled release, with the aim to quantify and potentially locate the emissions using flux footprint analysis. The EC tower was set up 26.4 m north-east of the injection point. Methane fluxes as high as 0.22 µmol m⁻² s⁻¹ were observed during the injection period when wind was from the injection area. Additionally, continuous CO₂ and H₂O fluxes were measured using an enclosed-path infrared gas analyzer, LI-7200 (LI-COR Inc.). A set of climate instruments including soil and radiation sensors were also installed to monitor weather conditions and energy balance closure. Down-scaling the EC fluxes to quantify emissions indicated that the volume released into the atmosphere ranged from 21.9 m³ to 24.6 m³. However, it was conjectured that this could be an underestimate because flux footprint models are applied to releases occurring at the ground and not at a height above the surface, and in this case, there was evidence that most of the emissions were from a ~1-m high well-head. The results suggest the need for an alternate flux footprint model, which considers the height of the source. Furthermore, an inversion approach was tested in an attempt to locate the leak and the results were compared with the original information about the location of the leak, as observed using chamber measurements and a groundwater sampling well. A point source controlled-release experiment was also conducted by releasing 93% v/v methane into the atmosphere to evaluate the flux footprint models being used in this study.
Agricultural fields are significant sources of carbon dioxide (CO₂), nitrous oxide (N₂O) and methane (CH₄), which has implications for future climate change. In Canada, studies incorporating all three greenhouse gases (GHGs) in agricultural settings are limited to Ontario, Quebec and the Prairies and generally involve short-duration static-chamber measurements. Results from these studies may not generalize well to British Columbia (BC) on the west coast, which has a milder climate and different cropping systems. This study quantified year-round (January 1, 2018 – December 31, 2018) CO₂, N₂O and CH₄ exchange over a conventionally managed highbush blueberry field on Westham Island in Delta, BC, Canada using the eddy-covariance (EC) method. Continuous measurements using EC allowed for quantification of diurnal courses of both CO₂ and N₂O exchange, whereas sporadic measurements may not accurately reproduce the complete diurnal cycle of GHG emissions. Sawdust mulching may have contributed to a reduction in evapotranspiration but has implications for increased CO₂ and N₂O emissions. Field management including fertilization and mowing was associated with substantial changes in GHG exchange, suggesting that management strategies can be targeted for potential GHG mitigation. The field was a net source of all measured GHGs and emitted 838 g CO₂e m-² year-¹, with CO₂ contributing the largest proportion (76%) followed by N₂O (20%) and CH4 (4%). The annual net ecosystem exchange (NEE) was 173 g C m-² year-¹ with the ratio of annual gross primary productivity (GPP) to ecosystem respiration (Re) being 0.88. After accounting for inputs and outputs of carbon (C), the field sequestered a net of 231 g C m-² year-¹. While soil temperature was found to be an important environmental factor controlling GHG emissions, soil moisture was also found to be an important factor, which has implications on future feedback cycles and climate change.
Hybrid poplar (HP) plantations established on former agricultural land in the aspen parkland of Canada have the potential to provide fibre, bio-energy and ecosystem services. The low precipitation and large summertime vapor pressure deficits in the aspen parkland raise questions about HP plantation water use and its effects on regional water supplies. In 2010 and 2011, I began using the eddy-covariance (EC) technique to measure CO₂, water vapor and sensible heat fluxes above two young HP plantations planted in 2009 (HP09) and 2011 (HP11) on clay loam Chernozemic soil located near Edmonton, AB and Winnipeg, MB, respectively. Measurements showed that both HP09 and HP11 shifted from carbon (C) sources to C sinks in the 3rd year of growth. EC measured evapotranspiration (E) and climate data were used to calculate bulk surface conductance (Gs) using the inverted Penman-Monteith (PM) equation and were compared to Gs estimates derived from a biophysical model that permits the partitioning of E into canopy transpiration (Ec) and evaporation from the soil (Es). Es was estimated using the equilibrium evaporation rate modified to account for soil moisture effects on Es using a soil water content based multiplier (f), and Ec was estimated using a canopy conductance (Gc) sub-model and the PM equation. Modelled half-hourly values of Gs showed excellent diurnal and seasonal agreement with EC-calculated Gs. Measured and modelled E also had excellent agreement, and using the Gs model, I was able to show the relative contribution of Ec and Es to E as the plantation grew. For example, in the 5th year of growth at HP09, measured and modelled E was 400 and 428 mm, respectively, of which 138 and 290 mm occurred as Es and Ec, respectively. Values of water use efficiency calculated as gross primary productivity divided by E, increased every year of growth and were similar at both sites. Results show Es dominates E during the first 2 years of HP growth and as Ec becomes increasingly dominant in the following years, E can exceed P, suggesting HP planted on highly productive agricultural soils in Canada’s aspen parkland can become water limited.
The recent mountain pine beetle (MPB) outbreak has had a major impact on the carbon (C) cycling of lodgepole pine forests in British Columbia. Mitigation efforts to control the insect outbreak have led to increased harvesting rates in the province. This study determines whether partial harvesting as an alternative forest management response to clearcutting can increase the net ecosystem production (NEP) of a mixed conifer forest (MPB-09) in Interior BC. Using the eddy-covariance (EC) technique, the C dynamics of the 70-year old stand were studied over the two years after partial harvest following MPB attack and also compared to an adjacent clearcut (MPB-09C) over the growing season. The annual NEP at MPB-09 increased from -107 g C m⁻² in 2010 to -57g C m⁻² in 2011. The increase of NEP was because the associated increase in annual gross ecosystem photosynthesis (GEP) from 812 g C m⁻² in 2010 to 954 g C m⁻² in 2011 exceeded the increase in annual respiration (Re) from 920 g C m⁻² to 1011 g C m⁻² in the two years of study. During the growing season of 2010, NEP at MPB-09C was -132 g C m⁻² indicating high C losses in the clearcut. MPB-09 was a C sink during the growing season of both years, increasing from 9 g C m⁻² in 2010 to 47 g C m⁻² in 2011. The increase of NEP in the partially harvested forest suggests stand recovery following harvest, which corresponds to a 25% increase in the maximum assimilation rate in the second year. This study shows that retaining the healthy residual forest can greatly enhance the C sequestration of MPB-attacked stands and has important implications for forest management.