Nitrogen Cycles: Past, Present, and Future

This paper contrasts the natural and anthropogenic controls on the conversion of unreactive N₂ to more reactive forms of nitrogen (Nr). A variety of data sets are used to construct global N budgets for 1860 and the early 1990s and to make projections for the global N budget in 2050. Regional N budgets for Asia, North America, and other major regions for the early 1990s, as well as the marine N budget, are presented to Highlight the dominant fluxes of nitrogen in each region. Important findings are that human activities increasingly dominate the N budget at the global and at most regional scales, the terrestrial and open ocean N budgets are essentially disconnected, and the fixed forms of N are accumulating in most environmental reservoirs. The largest uncertainties in our understanding of the N budget at most scales are the rates of natural biological nitrogen fixation, the amount of Nr storage in most environmental reservoirs, and the production rates of N₂ by denitrification.     

模拟地表火行为对燃烧剩余物水溶性碳氮的影响

燃烧剩余物是火烧迹地土壤表面必然存在的残留物,可以通过降水过程以及地表径流释放其所含有的矿物质和有机质至土壤生态系统,从而在一定时间内持续地对火后生态系统恢复过程造成影响。但不同火行为下,相同的可燃物所产生的燃烧剩余物可能具有不同的生态学功能,为了认知火行为对燃烧剩余物的影响,进一步了解二者对火烧迹地生态恢复过程中养分循环和能量流动的潜在影响,探究了火行为对燃烧剩余物水溶性碳氮化学计量特征的影响。以红松人工林地表可燃物为实验材料,通过设置不同坡度和含水率为火行为的驱动因子,进行了森林可燃物床层地表上坡火和下坡火的室内模拟燃烧实验。用独立样本T检验、单因素方差分析、多因素方差分析探究了火环境对燃烧剩余物水溶性碳氮和火行为的影响,用基于距离的冗余分析(db-RDA)探究了火行为对燃烧剩余物水溶性碳氮化学计量特征的影响。上坡火实验组的燃烧剩余物水溶性碳氮含量明显高于下坡火实验组(P<0.01);5°实验组中,燃烧剩余物的水溶性碳含量随着可燃物预设含水率的升高而升高(P<0.05)。进一步的数据分析发现火行为与燃烧剩余物水溶性碳氮化学计量特征关系密切,火焰宽度是影响燃烧剩余物水溶性...     

Cross‐scale controls on carbon emissions from boreal forest megafires

Climate warming and drying is associated with increased wildfire disturbance and the emergence of megafires in North American boreal forests. Changes to the fire regime are expected to strongly increase combustion emissions of carbon (C) which could alter regional C balance and positively feedback to climate warming. In order to accurately estimate C emissions and thereby better predict future climate feedbacks, there is a need to understand the major sources of heterogeneity that impact C emissions at different scales. Here, we examined 211 field plots in boreal forests dominated by black spruce (Picea mariana) or jack pine (Pinus banksiana) of the Northwest Territories (NWT), Canada after an unprecedentedly large area burned in 2014. We assessed both aboveground and soil organic layer (SOL) combustion, with the goal of determining the major drivers in total C emissions, as well as to develop a high spatial resolution model to scale emissions in a relatively understudied region of the boreal forest. On average, 3.35 kg C m^?2 was combusted and almost 90% of this was from SOL combustion. Our results indicate that black spruce stands located at landscape positions with intermediate drainage contribute the most to C emissions. Indices associated with fire weather and date of burn did not impact emissions, which we attribute to the extreme fire weather over a short period of time. Using these results, we estimated a total of 94.3 Tg C emitted from 2.85 Mha of burned area across the entire 2014 NWT fire complex, which offsets almost 50% of mean annual net ecosystem production in terrestrial ecosystems of Canada. Our study also highlights the need for fine‐scale estimates of burned area that represent small water bodies and regionally specific calibrations of combustion that account for spatial heterogeneity in order to accurately model emissions at the continental scale.     

Mechanistic studies of sesquiterpene cyclases based on their carbon isotope ratios at natural abundance

During the process of terpene biosynthesis, C–C bond breaking and forming steps are subjected to kinetic carbon isotope effects, leading to distinct carbon isotopic signatures of the products. Accordingly, carbon isotopic signatures could be used to reveal the ‘biosynthetic history’ of the produced terpenoids. Five known sesquiterpene cyclases, regulating three different pathways, representing simple to complex biosynthetic sequences, were heterologously expressed and used for in vitro assays with farnesyl diphosphate as substrate. Compound specific isotope ratio mass spectrometry measurements of the enzyme substrate farnesyl diphosphate (FDP) and the products of all the five cyclases were performed. The calculated δ¹³C value for FDP, based on δ¹³C values and relative amounts of the products, was identical with its measured δ¹³C value, confirming the reliability of the approach and the precision of measurements. The different carbon isotope ratios of the products reflect the complexity of their structure and are correlated with the frequency of carbon–carbon bond forming and breaking steps on their individual biosynthetic pathways. Thus, the analysis of carbon isotopic signatures of terpenes at natural abundance can be used as a powerful tool in elucidation of associated biosynthetic mechanisms of terpene synthases and in future in vivo studies even without ‘touching’ the plant.     

Radical Formation from the Reaction of Combustion Smoke with Diphenylamine

We have attempted to examine the effects of radical scavengers, such as amines and phenols, to trap gasphase radicals produced from the combustion of Poly (methyl methacrylate)(PMMA), which might cause damage to a living body, using an electron spin resonance (ESR) spin-trapping technique.

As a result, diphenylamine did not decrease the amount of radicals but rather increased it. It indicates that under the conditions of this study, gas-phase radicals were hardly trapped by radical scavengers and that the precursors to produce other kinds of radicals can exist.

It was suggested that from the experiments using several peroxides, the precursors should be diacylperoxides produced from the combustion of PMMA.     

Structure and photoluminescent properties of green‐emitting terbium‐doped GdV1−xPxO4 phosphor prepared by solution combustion method

Terbium‐doped gadolinium orthovanadate (GdVO₄:Tb³⁺), orthophosphate monohydrate (GdPO₄·H₂O:Tb³⁺) and orthovanadate–phosphate (GdV,PO₄:Tb³⁺) powder phosphors were synthesized using a solution combustion method. X‐Ray diffraction analysis confirmed the formation of crystalline GdVO₄, GdPO₄·H₂O and GdV,PO₄. Scanning electron microscopy images showed that the powder was composed of an agglomeration of particles of different shapes, ranging from spherical to oval to wire‐like structures. The chemical elements present were confirmed by energy dispersive spectroscopy, and the stretching mode frequencies were determined by Fourier transform infrared spectroscopy. UV–visible spectroscopy spectra showed a strong absorption band with a maximum at 200 nm assigned to the absorption of VO₄^3? and minor excitation bands assigned to f → f transitions of Tb³⁺. Four characteristic emission peaks were observed at 491, 546, 588 and 623 nm, and are attributed to ⁵D₄ → ⁷F_j (j = 6, 5, 4 and 3). The photoluminescent prominent green emission peak (⁵D₄ → ⁷F₅) was centred at 546 nm. The structure and possible mechanism of light emission from GdV_1?xP_xO₄:% Tb³⁺ are discussed. Copyright © 2016 John Wiley & Sons, Ltd.     

Dependence on growth phase and temperature of the composition of a nitrogen-fixing cyanobacterium

The effects of growth pahase and temperature on the molecular and elemental composition of Anabaena variabilis cells grown under nitrogen-fixing conditions have been studied in batch cultures. Irrespective of the growth temperature, this cyanobacterium underwent a gradual increase in its protein and lipid contents in the transition from exponential to deceleration pahse that was accompanied by a parallel decrease in carbohydrates and nucleic acids. Also in response to this, transition increases in carbon, nitrogen, and hydrogen contents with a concomitant decline in oxygen content was a common pattern for all growth temperatures tested. Whereas temperature rise did not affect significantly the protein and carbohydrate contents in exponentially growing cells, for cells in the deceleration phase proteins declined and carbohydrates increased with increasing temperature. From growth and elemental composition data several bioenergetic parameters were derived for A. variabilis cells. Both aging of cultures and rise in temperature resulted in increases of both biomass degree of reduction and heat of combustion. Nevertheless, biomass energetic yield was only slightly affected by variations in growth temperature and the maintenance coefficient was virtually constant within the range of temperatures tested. (c) 1992 John Wiley & Sons, Inc.     

Synthesis of the long‐persistence phosphor CaAl2O4:Eu2+, Dy3+, Nd3+ by combustion method and its luminescent properties

Calcium aluminate phosphor co‐doped Eu²⁺, Dy³⁺, Nd³⁺ is prepared by the combustion method. We study systemically the influences of the quantity of mixed Dy³⁺ ion, the quantity of flux H₃BO₃, the differences in dispersing methods between magnetic stirring and ultrasonic dispersing and the combustion temperature on the long‐persistence phosphor. The analytical results indicate that Dy³⁺ ion improves the properties of the phosphors CaAl₂O₄:Eu²⁺, Nd³⁺. The appropriate quantity of flux H₃BO₃ to reduce the forming temperature of the sample was determined. The monoclinic single phase of CaAl₂O₄ formed at 500°C and remained steady. The calcium aluminate co‐doped Eu²⁺, Dy³⁺, Nd³⁺ was synthesized by dispersal of the raw material using the ultrasonic method, and it had better optical properties. Copyright © 2009 John Wiley & Sons, Ltd.     

Effects of wildfire and permafrost on soil organic matter and soil climate in interior Alaska

The influence of discontinuous permafrost on ground‐fuel storage, combustion losses, and postfire soil climates was examined after a wildfire near Delta Junction, AK in July 1999. At this site, we sampled soils from a four‐way site comparison of burning (burned and unburned) and permafrost (permafrost and nonpermafrost). Soil organic layers (which comprise ground‐fuel storage) were thicker in permafrost than nonpermafrost soils both in burned and unburned sites. While we expected fire severity to be greater in the drier site (without permafrost), combustion losses were not significantly different between the two burned sites. Overall, permafrost and burning had significant effects on physical soil variables. Most notably, unburned permafrost sites with the thickest organic mats consistently had the coldest temperatures and wettest mineral soil, while soils in the burned nonpermafrost sites were warmer and drier than the other soils. For every centimeter of organic mat thickness, temperature at 5 cm depth was about 0.5°C cooler during summer months. We propose that organic soil layers determine to a large extent the physical and thermal setting for variations in vegetation, decomposition, and carbon balance across these landscapes. In particular, the deep organic layers maintain the legacies of thermal and nutrient cycling governed by fire and revegetation. We further propose that the thermal influence of deep organic soil layers may be an underlying mechanism responsible for large regional patterns of burning and regrowth, detected in fractal analyses of burn frequency and area. Thus, fractal geometry can potentially be used to analyze changes in state of these fire prone systems.     

Policy implications of human-accelerated nitrogen cycling

The human induced input of reactive N into the globalbiosphere has increased to approximately 150 Tg N eachyear and is expected to continue to increase for theforeseeable future. The need to feed (125 Tg N) andto provide energy (25 Tg N) for the growing worldpopulation drives this trend. This increase inreactive N comes at, in some instances, significantcosts to society through increased emissions of NO_x,NH₃, N₂O and NO₃ ^– and deposition of NO_y and NH_x.In the atmosphere, increases in tropospheric ozone andacid deposition (NO_y and NH_x) have led toacidification of aquatic and soil systems and toreductions in forest and crop system production. Changes in aquatic systems as a result of nitrateleaching have led to decreased drinking water quality,eutrophication, hypoxia and decreases in aquatic plantdiversity, for example. On the other hand, increaseddeposition of biologically available N may haveincreased forest biomass production and may havecontributed to increased storage of atmospheric CO₂ inplant and soils. Most importantly, syntheticproduction of fertilizer N has contributed greatly tothe remarkable increase in food production that hastaken place during the past 50 years.The development of policy to control unwanted reactiveN release is difficult because much of the reactive Nrelease is related to food and energy production andreactive N species can be transported great distancesin the atmosphere and in aquatic systems. There aremany possibilities for limiting reactive N emissionsfrom fuel combustion, and in fact, great strides havebeen made during the past decades. Reducing theintroduction of new reactive N and in curtailing themovement of this N in food production is even moredifficult. The particular problem comes from the factthat most of the N that is introduced into the globalfood production system is not converted into usableproduct, but rather reenters the biosphere as asurplus. Global policy on N in agriculture isdifficult because many countries need to increase foodproduction to raise nutritional levels or to keep upwith population growth, which may require increaseduse of N fertilizers. Although N cycling occurs atregional and global scales, policies are implementedand enforced at the national or provincial/statelevels. Multinational efforts to control N loss tothe environment are surely needed, but these effortswill require commitments from individual countries andthe policy-makers within those countries.