Exam 54: Ecosystems

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Figure 54.9 Figure 54.9   -Which of the following is not a source of human-fixed nitrogen? -Which of the following is not a source of human-fixed nitrogen?

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Figure 54.1 -How are the components in Figure 54.1 linked by the flow of energy? Figure 54.1 -How are the components in Figure 54.1 linked by the flow of energy?    Figure 54.1 -How are the components in Figure 54.1 linked by the flow of energy?

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Use the following information when answering the corresponding question(s). Abstract: Increased radiative forcing is an inevitable part of global climate change,yet little is known of its potential effects on the energy fluxes in natural ecosystems.To simulate the conditions of global warming,we exposed peat monoliths (depth,0.6 cm;surface area,2.1 m²)from a bog and fen in northern Minnesota,USA,to three infrared (IR)loading (ambient,+45,and +90 W m⁻²)and three water table (-16,-20,and -29 cm in bog and -1,-10 and -18 cm in fen)treatments,each replicated in three mesocosm plots.Net radiation (Rn)and soil energy fluxes at the top,bottom,and sides of the mesocosms were measured in 1999,five years after the treatments had begun.Soil heat flux (G)increased proportionately with IR loading,comprising about 3%-8% of Rn.In the fen,the effect of IR loading on G was modulated by water table depth,whereas in the bog,it was not.Energy dissipation from the mesocosms occurred mainly via vertical exchange with air,as well as the deeper soil layers through the bottom of the mesocosms,whereas lateral fluxes were 10- to 20-fold smaller and independent of IR loading and water table depth.The exchange with deeper soil layers was sensitive to water table depth,in contrast to G,which responded primarily to IR loading.The qualitative responses in the bog and fen were similar,but the fen displayed wider seasonal variations and greater extremes in soil energy fluxes.The differences of G in the bog and fen are attributed to differences in the reflectance in the long waveband as a function of vegetation type,whereas the differences in soil heat storage may also depend on different soil properties and different water table depth at comparable treatments.These data suggest that the ecosystem-dependent controls over soil energy fluxes may provide an important constraint on biotic response to climate change. -The Noormets et al.study (2004)shows that there was an ecosystem-specific control over soil energy fluxes,and this constrained the biotic response to climate change.How do you think radiative heat would affect the water table in a wetland versus a temperate forest?

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What do researchers typically focus on when they study a particular biogeochemical cycle?

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Figure 54.4 Figure 54.4   -What is the main reason for using food webs instead of food chains in analyzing ecosystems? -What is the main reason for using food webs instead of food chains in analyzing ecosystems?

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Figure 54.5 Figure 54.5   -If plants in a northern temperate area use 26,400 kcal/m² of energy from solar radiation in photosynthesis,and the total amount of solar radiation energy reaching that area is 2,640,000 kcal/m²,what is the overall gross photosynthetic efficiency? -If plants in a northern temperate area use 26,400 kcal/m² of energy from solar radiation in photosynthesis,and the total amount of solar radiation energy reaching that area is 2,640,000 kcal/m²,what is the overall gross photosynthetic efficiency?

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Figure 54.3 Figure 54.3   -Considering its total area covered,which ecosystem type represented in Figure 54.3 has a very low level of economic impact on Earth's ecosystem? -Considering its total area covered,which ecosystem type represented in Figure 54.3 has a very low level of economic impact on Earth's ecosystem?

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Figure 54.5 Figure 54.5   -After looking at Figure 54.5,what can be said about productivity in this ecosystem? -After looking at Figure 54.5,what can be said about productivity in this ecosystem?

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Figure 54.5 Figure 54.5   -Plants never use 100% of the incoming solar radiation for photosynthesis on a yearly basis.What is a reasonable explanation for this? -Plants never use 100% of the incoming solar radiation for photosynthesis on a yearly basis.What is a reasonable explanation for this?

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Figure 54.9 Figure 54.9   -Considering the global nitrogen cycle,how are humans altering this cycle? -Considering the global nitrogen cycle,how are humans altering this cycle?

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Figure 54.7 Figure 54.7   -Based on the experiment in Figure 54.7,all of the following are plausible reasons for the result except _____. -Based on the experiment in Figure 54.7,all of the following are plausible reasons for the result except _____.

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Figure 54.3 Figure 54.3   -Which habitat types in Figure 54.3 cover the largest area? -Which habitat types in Figure 54.3 cover the largest area?

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Use the following information when answering the corresponding question(s). Abstract: Increased radiative forcing is an inevitable part of global climate change,yet little is known of its potential effects on the energy fluxes in natural ecosystems.To simulate the conditions of global warming,we exposed peat monoliths (depth,0.6 cm;surface area,2.1 m²)from a bog and fen in northern Minnesota,USA,to three infrared (IR)loading (ambient,+45,and +90 W m⁻²)and three water table (-16,-20,and -29 cm in bog and -1,-10 and -18 cm in fen)treatments,each replicated in three mesocosm plots.Net radiation (Rn)and soil energy fluxes at the top,bottom,and sides of the mesocosms were measured in 1999,five years after the treatments had begun.Soil heat flux (G)increased proportionately with IR loading,comprising about 3%-8% of Rn.In the fen,the effect of IR loading on G was modulated by water table depth,whereas in the bog,it was not.Energy dissipation from the mesocosms occurred mainly via vertical exchange with air,as well as the deeper soil layers through the bottom of the mesocosms,whereas lateral fluxes were 10- to 20-fold smaller and independent of IR loading and water table depth.The exchange with deeper soil layers was sensitive to water table depth,in contrast to G,which responded primarily to IR loading.The qualitative responses in the bog and fen were similar,but the fen displayed wider seasonal variations and greater extremes in soil energy fluxes.The differences of G in the bog and fen are attributed to differences in the reflectance in the long waveband as a function of vegetation type,whereas the differences in soil heat storage may also depend on different soil properties and different water table depth at comparable treatments.These data suggest that the ecosystem-dependent controls over soil energy fluxes may provide an important constraint on biotic response to climate change. -Once heat is transferred to the soil,where does it go afterward (Noormets et al.2004)?

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Figure 54.3 Figure 54.3   -Which category in Figure 54.3 makes available the highest productivity per square meter? -Which category in Figure 54.3 makes available the highest productivity per square meter?

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Figure 54.4 Figure 54.4   -Detritus can be consumed by which of the following primary decomposers? -Detritus can be consumed by which of the following primary decomposers?

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Figure 54.8 Figure 54.8   -Which of the following human activities is impacting the water cycle the least? -Which of the following human activities is impacting the water cycle the least?

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Figure 54.5 Figure 54.5   -Why is energy lost when herbivores eat primary producers? -Why is energy lost when herbivores eat primary producers?

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At the Hubbard Brook Experimental Forest in New Hampshire,how did large amounts of energy leave the decomposer food web?

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You own 300 acres of patchy temperate forest.Which one of the following actions would increase the net primary productivity of the area the most?

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Figure 54.6 Figure 54.6   -Which of the following statements about secondary production is true? -Which of the following statements about secondary production is true?

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