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Leaf traits have long been used to classify and characterise species in natural ecosystems. In addition, leaf traits provide important information about plants’ strategies for the use of resources and can be used to improve our understanding of ecosystem level processes such as nutrient cycling and carbon allocation. To explore the linkages between leaf traits and productivity, we worked in two resource-limited ecosystems (a grassland and a forest), and used leaf traits to understand how species respond to changes in available resources and their relationship to ecosystem processes. We worked in a species rich limestone-grassland located in central England, which has been subjected to long-term climatic manipulation (winter warming, summer drought and extra summer rainfall). We characterised species composition in terms of their identity, abundance and leaf structural properties (nitrogen content and leaf mass per area (LMA)) in the main treatments and the control. We found that change in species abundance was the most important factor to understand the differences in productivity (above ground biomass and total foliar nitrogen). We then measured CO2 exchange at ecosystem level, using a chamber technique, and assessed the treatments’ effect on the gross primary productivity (GPP) and ecosystem respiration (Reco). GPP and Reco were controlled by soil moisture and above ground biomass but also influenced by the conditions experienced during the growing season prior to the measuring period. Our second location was a post-disturbance chronosequence in a seasonally dry tropical forest in Costa Rica and we used leaf level gas exchange measurements to explore the role of nitrogen (N) and phosphorus (P) on the temporal-spatial variation of photosynthesis of dominant species. We found that photosynthetic efficiency was strongly linked to leaf N and P content, but that there was an important seasonal pattern on this relationship likely associated to P remobilization. Additionally we found seasonal changes in resources (water, nutrients) had a larger impact on the photosynthetic parameters than changes along the chronosequence. The two ecosystems studied for this thesis are contrasting in their physiognomy, species composition and climate, but are also characterised by species whose structural traits (high LMA and high C:N ratio) are likely to have a significant impact on the nutrient cycling processes. We learned that leaf traits provide important information about species strategies and their usage of resources and they can also aid to address questions at ecosystem level in time and space, either through simple aggregation or as emergent properties. Additionally, the traits explored are important input information to up-scale processes from leaf to the ecosystem level, a step needed to address the effect changes in resources will have on the seasonally dry tropical forest and grasslands, which represent a significant fraction of the total global carbon storage.

Doctor of Philosophy / Department of Agronomy / Ganga M. Hettiarachchi / Although phosphorus (P) is an essential nutrient for the growth of plants, it is one of the most limiting nutrients in terms of availability as a high proportion of applied P rapidly transforms into insoluble forms with low solubility in soils. To further understand the fate of P applied to soils, two separate but related studies using three high P-fixing soil types each were used for which the objectives were to investigate the mobility, availability, and reaction products from two granular and one liquid P fertilizer alone or plus a fertilizer enhancement product. Energy dispersive spectroscopy showed a substantial amount of P remained in the granule following a 5-week incubation. At the end of the 35-day incubation period there was evidence that the fluid fertilizer was superior over the granular sources in terms of enhanced diffusion and extractability of P for three calcareous soils with varying levels of CaCO3. Phosphorus x-ray absorption near-edge structure (XANES) spectroscopy results in conjunction with resin-extractable P indicated a strong negative correlation between Ca-P solids formed and P extractability, suggesting that degree of Ca-P formation limits P solubility. For the three acidic P-fixing soils the results were complex. In two out of three acid soils, liquid P treatments diffused farther from the application point than the granular treatments. Phosphorus XANES results suggested that Fe-P or Al-P interactions control the overall P solubility. Integration of pH, resin extractable-P and XANES results suggested the P retention mechanism was either dominated by adsorption or precipitation depending on soil pH. More acidic soil conditions favored precipitation. The objectives of the third study were to observe how long-term (14 years) addition of P with or without N influences the inorganic and organic P pools in a native grassland soil using sequential fractionation, XANES, and 31P-nuclear magnetic resonance (NMR) spectroscopy. The overall results suggested that P and N fertilization and associated changes in plant productivity induced significant changes in soil P pools such as Ca-P, phytic acid, monoesters, and residual forms of P. The addition of P alone induced formation of inorganic P forms while the addition of P and N induced transformation of residual P forms into more labile and/or organic P forms.

Estudos bioestratigráficos, com base em nanofósseis calcários de amostras provenientes do DSDP, Leg 40, poços 364 e 361, das Bacias de Angola - Cuanza e Cabo - Orange, na Margem Africana, permitiram o refinamento taxonômico, para o Período Cretáceo (145,5 - 65,5 M.a.), entre os andares Aptiano e Turoniano (125 - 89,3 M.a.). Os dados do Leg 40 obtidos pelos relatórios do DSDP, na década de 1970, foram confeccionados sobre uma bibliografia controversa, utilizando biozoneamentos de regiões distintas do Oceano Atlântico Sul. No poço 364, 89% das amostras continham material passível de análise, totalizando 168 lâminas úteis para a obtenção das informações bioestratigráficas. Foram identificados um total de 78 taxa de nanofósseis calcários, com 66 a nível de espécie e 12 a nível de gênero. No poço 361, 67% das amostras apresentaram conteúdo afossilífero, e assim foram confeccionadas 64 lâminas, onde identificou-se 18 taxas, sendo 9 a nível espécie, 6 a nível gênero e 3 a nível família. O refinamento bioestratigráfico realizado possibilitou dividir, no poço 364, a seção cretácea amostrada em cinco andares, sendo eles: Turoniano (93,5 - 89,3 M.a.), Cenomaniano (99,6 - 93,5 M.a.), Albiano (112 - 99,6 M.a.), Aptiano (125 - 112 M.a.) e um identificado genericamente como Cretáceo inferior (de 125 M.a. para a base). No poço 361, a divisão do nível Cretáceo amostrado se deu em três andares: Um Albiano (112 - 99,6 M.a.), outro Aptiano (125 - 112 M.a.) e um Cretáceo genérico (de 125 M.a. para a base). Com os dados bioestratigráficos obtidos nos dois poços, foi possível gerar uma correlação entre ambos poços, integrando os andares Albiano (112 - 99,6 M.a.) e Aptiano (125 - 112 M.a.). Tal correlação permitiu interpretar em qual momento houve a influência das águas advindas do norte (Bacia de Angola - Cuanza) e do sul (Bacia do Cabo - Orange), divididas pelo alto estrutural representado pela Cordilheira de Walvis. / Biostratigraphic studies, based on calcareous nanofossils samples from DSDP, Leg 40, sites 364 and 361 (Angola - Cuanza and Cabo - Orange Basins, African Margin), allowed the taxonomic refinement for the Cretaceous period (145.5 - 65.5 M.a.), between Aptian and Turonian (125 - 89.3 M.a.). The Leg 40 data obtained from the 1970\'s DSDP reports were based in a controversial literature using biozones from distinct regions of the South Atlantic Ocean. In site 364, 89% of the samples contained nanofossil material, counting 168 slides useful to obtain biostratigraphic information. 78 taxa of calcareous nanofossils were identified, 66 at specific level and 12 at generic level. In site 361, 67% of the samples were sterile, thus, 64 slides were made, where 18 taxa were identified, 9 at the specific level, 6 at generic level and 3 at family level. The biostratigraphic refinement allowed to divide the Cretaceous section sampled on five ages in site 364: Turonian (93.5 - 89.3 Ma), Cenomanian (99.6 - 93.5 Ma), Albian (112 - 99.6 Ma), Aptian (125 - 112 Ma) and one generally identified as Lower Cretaceous (125 M.a. down). At site 361, the division of the Cretaceous level sampled occurred in three ages: Albian (112 - 99.6 M.a.), Aptian (125 - 112 M.a.) and a Cretaceous generic (125 M.a. down). With the biostratigraphic data obtained in the two sites, it was possible to generate a correlation between both sites, integrating the Albian (112 - 99.6 M.a.) and Aptian (125 - 112 M.a.) ages. This correlation made it possible to interpret the influence of waters from the north (Angola - Cuanza Basin) and the South (Cape Basin - Orange), divided by the structural high represented by the Walvis Ridge.

O objetivo do presente estudo foi estimar as possíveis variações na produtividade das águas superficiais da porção oeste do oceano Atlântico Sul ao longo dos últimos 15.000 anos, contribuindo para a melhor compreensão das variações oceanográficas ocorridas na região no decorrer deste tempo. Foram realizadas análises quantitativas de nanofósseis calcários em um testemunho da Bacia de Santos, a partir da técnica de decantação aleatória. Isótopos estáveis de carbono e oxigênio em rocha total e teor de carbonato de cálcio também foram utilizados para interpretações sobre paleoprodutividade. A produtividade primária das águas superficiais apresentou variações ao longo dos últimos 15.000 anos. Variações no aporte continental e na profundidade da termoclina/nutriclina devem ter influenciado as condições das águas superficiais da região, e conseqüentemente, a produtividade dos cocolitoforídeos. Estimou-se que a produtividade da camada fótica superior tenha diminuído desde o início do Holoceno. Anterior a este período, uma maior contribuição continental teria propiciado condições mais favoráveis ao desenvolvimento dos cocolitoforídeos que habitam as camadas mais superficiais do oceano. / The aim of this study consisted in estimate possible changes on southwestern Atlantic Ocean surface water productivity for the last 15.000 years, contributing to a better understanding of oceanographic changes that occurred along this time. Quantitative calcareous nannofossils analyses were carried out on a Santos Basin core using the random settling technique. Bulk carbon and oxygen stable isotopes and calcium carbonate content were also used for paleoproductivity interpretation. Primary productivity of surface waters presented variation along the last 15.000 years. Variations in continental contribution and thermocline/nutricline depth must have influenced the surface water conditions and therefore coccolithophorids productivity. Upper photic zone productivity was estimated and seems to have diminished since early Holocene. Prior to this time, a major continent contribution would have provided more favorable conditions for the development of the coccolithophorids that inhabit the upper layers of the ocean.

Atualmente a ordem Dendrochirotida é composta por 800 espécies, sendo que metade destas estão entre as famílias Sclerodactylidae e Phyllophoridae. Todavia, a maior parte das informações acerca dos seus táxons é proveniente de revisões morfológicas muito antigas (Phyllophoridae em 1954, e Sclerodactylidae não revisada). Este estudo, portanto, se configura como o primeiro teste formal da monofilia das famílias Sclerodactylidae e Phylllophoridae e suas subfamílias. O presente trabalho constitui um estudo morfológico minucioso das estruturas que compõem o endoesqueleto dos Holothuroidea que são os ossículos dérmicos e anel calcário, vislumbrando alcançar através de uma análise cladística os objetivos descritos a seguir: (i) testar a monofilia de Phyllophoridae; (ii) testar a monofilia de Sclerodactylidae; (iii) testar a monofilia das subfamílias de Phyllophoridae e (iv) testar a monofilia das subfamílias de Sclerodactylidae. O material estudado foi obtido a partir de visitas e/ou empréstimos de museus nacionais e internacionais. Foram estudados espécimes de todas as ordens de Holothuroidea, à exceção de Elasipodida, totalizando 956 espécimes pertencentes a 78 espécies, das quais quatro foram delimitadas como grupo externo (i.e. Aspidochirotida, Apodida e Dendrochirotida [Cucumariidae e Psolidae]) e 44 delimitadas como grupo interno (todas as espécies tipo foram analisadas). Setenta e dois caracteres foram descritos e ilustrados através de fotografias ou microscopia eletrônica de varredura. As análises foram realizadas com o programa PAUP (v. 4.0), através do algoritmo de parcimônia Tree Bissection and Reconnection (TBR) de branch-swapping, com 5000 réplicas. O estudo morfológico detalhado permitiu elencar novos caracteres, bem como reinterpretar caracteres já estabelecidos, além de fornecer correções de interpretações equivocadas acerca de tais estruturas. Sclerodactylidae foi recuperada como monofilética e está composta por três subfamílias (todas foram recuperadas como monofiléticas), Clado I, Sclerodactylinae e Thyoninae. Phyllophoridae foi recuperada como monofilética e está composta por três subfamílias (todas foram recuperadas como monofiléticas), Cladolabinae, Phyllophorinae e Semperiellinae. / Currently, the order Dendrochirotida comprises about 800 species, half of these being within the families Sclerodactylidae and Phyllophoridae. Regardless, most information about these families is from old morphological revisions (Phyllophoridae in 1954 and Sclerodactylidae not reviewed). This study appears as the first formal test of the monophyly of the families Sclerodactylidae and Phylllophoridae and their respective subfamilies. The present work constituted a detailed morphological study of the structures that compose the Holothuroidea endoskeleton which are the dermal ossicles and calcareous ring to achieve through a cladistic analysis the following objectives: (i) to test the monophyly of Phyllophoridae; (ii) to test the monophyly of Sclerodactylidae; (iii) to test the monophyly of the Phyllophoridae subfamilies and iv) to test the monophyly of the subfamilies of Sclerodactylidae. The material studied was obtained from visits and/or loans from the national and international museums. Specimens of all orders of Holothuroidea were analyzed with the exception of Elasipodida, yielding 956 specimens belonging to 78 species, of which four were delimited as outgroups (i.e. Aspidochirotida, Apodida and Dendrochirotida [Cucumariidae and Psolidae]) and 44 delimited as internal groups (all type specimens were analyzed). A total of 72 morphological characters were described and illustrated through photographs or scanning electron microscopy images. The analyses were conducted with the aid of PAUP (v.4.0) using a parsimony algorithm Tree Bisection and Reconnection (TBR) branch-swapping (5000 replicates). This detailed morphological study allowed us to list new characters, to reinterpret. already established ones as well as providing corrections of misinterpretations about such structures. Sclerodactylidae was recovered as monophyletic and is composed of three subfamilies (all were recovered as monophyletic), Clade I, Sclerodactylinae and Thyoninae. Phyllophoridae was recovered as monophyletic and consists of three subfamilies (all were recovered as monophyletic), Cladolabinae, Phyllophorinae and Semperiellinae.

Alumínio Pulverizado Termicamente (TSA) é amplamente utilizado em instalações offshore como revestimento de ânodo de sacrifício em tubulações de aço carbono. O transporte e a instalação desses componentes podem levar a pequenos danos no revestimento, o que pode expor a superfície do aço à água do mar. Sabe-se que o depósito calcário é formado na superfície do aço polarizado catodicamente. Assim, esta pesquisa avaliou o TSA aplicado por sistema de pulverização de arco duplo (TWAS) no aço ao carbono S355J2 + N quando ocorrem danos (holidays) para estudar a formação de depósitos calcários no aço e adquirir dados sobre o desempenho do TSA sob altas temperaturas. A aplicação de diferentes condições também foi considerada: presença de selantes; liga do revestimento (99,5% de Al e Al-5% de Mg) e condições enterradas/não enterradas. Dois tipos de experimentos foram realizados: i) testes em potencial livre sob temperaturas constantes (30, 60 e 90°C) e diferentes tamanhos de holidays (expondo 5, 10 e 20% da superfície do aço) e ii) testes sob gradient térmico onde óleo a ~125°C foi adicionado em uma torre polimérica e água externa a ~10°C ficou em contato com a superfície das amostras (tanto potencial livre como polarização de -950 mVAg/AgCl foram aplicados). Análises incluíram inspeção visual, microscópio eletrônico de varredura e difração de Raio-X. A partir dos testes em temperaturas constante, o TSA atingiu um bom potencial de proteção (-800 a -900 mVAg/AgCl) e pouca diferença nos resultados devido à diferença na composição doTSA e no tamanho do holiday foi observada. As taxas de corrosão foram mantidas entre 0,02 e 0,01 mm/ano. No ensaio sob gradiente térmico e potencial livre, a perda de revestimento e as taxas de corrosão foram de 0,4 a 0,002 mm/ano. Além disso, o potencial alcançado foi de uma faixa menor do que a obtida anteriormente (-745 a -835 mVAg/AgCl). No entanto, quando o TSA foi combinado com proteção catódica externa e gradiente térmico, a espessura do TSA foi satisfatório e as taxas de corrosão obtidas foram inferiores a 0,076 mm/ano. O depósito calcário formado no holiday protegeu o aço contra a corrosão e seu mecanismo de crescimento baseado nesta pesquisa foi construído. / Thermally Sprayed Aluminium (TSA) is widely used in offshore facilities as sacrificial anode coating for carbon-steel risers and pipelines. Transportation and installation of those components can lead to small damages in the coating, which can expose the steel surface to the seawater. It is known that calcareous deposit is formed on the cathodically polarised steel surface. Thus, this research evaluated the TSA applied by twin wire arc spray system (TWAS) on S355J2+N carbon-steel when damage (holidays) is present in order to study the calcareous deposit formation on steel and acquire data regarding the TSA performance at high temperatures. Application of different conditions was also considered: presence of sealing; coating alloy (99.5%Al and Al-5%Mg) and buried/unburied conditions. Generally, two types of experiment were conducted – i) tests at free potential at steady temperatures (30, 60 and 90°C) and different holiday sizes (exposing 5, 10 and 20% of the steel surface) and ii) tests under thermal gradient where oil at ~125°C was added in polymeric tower and external water at ~10°C was in contact with the samples surface (both free potential and polarisation of -950 mVAg/AgCl were applied). Methodology of analyses included visual inspection, scanning electron microscope and X-ray Diffraction. From the tests at steady temperatures, the TSA reached a very good protective potential (-800 to -900 mVAg/AgCl) and little difference in results due to difference in TSA composition and holiday size was observed. Corrosion rates were kept between 0.02 and 0.01 mm/year. From the thermal gradient test under free potential, the coating loss and corrosion rates were 0.4 to 0.002 mm/year. Also, the potential achieved was in a lower range than previously obtained (-745 to -835 mVAg/AgCl). However, when TSA was combined with external cathodic protection and thermal gradient, the thickness of the TSA was satisfactory and corrosion rates obtained were below 0.076 mm/year. The calcareous deposit formed within the holiday protected the steel substrate against corrosion and its growth mechanism based in this research was built.

Aflorando abundantemente nas drenagens da Serra da Bodoquena, região sudoeste do Estado de Mato Grosso do Sul, os depósitos de tufas calcárias, descritos como a porção superior da Formação Xaraiés, representam o mais notável depósito do tipo no Brasil, devido à variedade de formas. Sendo a maior atração do pólo eco-turístico de Bonito, MS, as tufas calcárias apresentam-se sob formas de barragens, cachoeiras e depósitos de micritos inconsolidados, que por sua vez geram as piscinas naturais e quedas dágua tão procuradas pelos turistas. Mesmo com tamanha importância, tal rocha não havia recebido um estudo aprofundando, que contemplasse sedimentologia, estratigrafia e geomorfologia. Através de criteriosa revisão bibliográfica, trabalhos em campo e análises laboratoriais, pôde-se obter um panorama da Formação Xaraiés na Serra da Bodoquena. Nesta região, observa-se que a formação, assentada diretamente sobre os calcários e dolomitos do Grupo Corumbá, sendo composta por um nível basal de calcretes, de tipo pedogenético e freático, sobreposto por um pacote de tufas micríticas (micrito inconsolidado), com grande quantidade de gastrópodes, distribuídos amplamente e aflorando em todas as planícies da região. Por fim temos os afloramentos de tufas calcárias do tipo fitohermal, compondo barragens e cachoeiras nas drenagens locais. Acredita-se que a deposição dos micritos ocorreu em ambiente lacustre, o que permitiu um depósito amplo e homogêneo, que posteriormente, em clima úmido, serviu de área fonte, juntamente com os carbonatos do Grupo Corumbá, para a geração das tufas fitohermais. A correlação estratigráfica dos depósitos de tufas calcárias estudados apontam para dois períodos de clima semi-árido a árido no Holoceno, que permitiram a formação e a alteração (calcretização) de depósitos, refletido na base da Formação Xaraiés, e o período climático recente, úmido, a formação das tufas fitohermais, no topo da formação. A ocorrência de lentes micríticas no sul do Pantanal pode significar que esta região também esteve exposta às dinâmicas climáticas vistas na Serra da Bodoquena. Estas constatações demonstram a alta variação climática da região, representada por depósitos que são pequenos e frágeis, mas dotados de significados genéticos indubitáveis. / Crop out abundantly in the Bodoquena Ridge drainages, southwest of Mato Grosso do Sul (MS) state, deposits of calcareous tufa were described as the top portion of Xaraiés Formation, representing the most notable deposit of this type in Brazil, due to the variety of forms. As the greatest attractiveness of Bonito, MS, an eco-tourism center, the calcareous tufa were presented in form of dams, waterfalls and deposits of micritic sediments, which generate natural pools and waterfalls so looked by tourists. Even with such importance, this region had not received a deep study, with sedimentology, stratigraphy and geomorphology approach. An accurate bibliographic review was done, and with field work and laboratory analyzes this work could obtain a panorama of the Xaraiés Formation in Bodoquena Ridge. In this region, can be noted that Xaraiés Formation goes directly over the limestone and dolomite of the Corumbá Group, and were composed by a basal layer of pedogenetic/groundwater calcrete, superimposed by a package of micritic sediments (micritic tufa), with a large amount of gastropods, which were widely distributed, cropping out in all plains of the region. Finally, we have the occurrences of calcareous tufa, fitohermal type, drawing dams and waterfalls in the regional drainages. It has believed that the deposition of lacustrine micritic sediments have occurred in an environment which were enabled a broad and homogeneous deposits. Subsequently, in a moister climate these sediments served as a source area, together with the limestone of the Corumbá Group, for the generation of fitohermal tufa. The stratigraphic correlation of the studied calcareous tufa deposits point to two periods of semi-arid/arid climate in Holocene, which allowed the calcretization. Those were reflected on the bottom of the Xaraiés Formation, and a recent wet climatic period, represented by the fitohermal tufa at the top of the formation. The occurrence of micritic lens in the southern Pantanal may mean that this region has also been exposed to the weather dynamics viewed in the Bodoquena Ridge. These findings show the high variation of climate in this region, represented by deposits, which are small and fragile, but gifted with unquestionable genetic meanings.

Soluble phosphorus fertilizer is bound in the soil rapidly after application in soils high in calcium. A fertilizer additive known as AVAIL® (J.R. Simplot Company) is purported to keep applied phosphorus fertilizer more available to plants by binding to soil minerals such as calcium, magnesium, and iron, thereby reducing phosphorus binding. This could prove useful due to the attraction of AVAIL® with cations such as Ca2+, but is fairly unstudied for dryland wheat production on alkaline, calcium-rich soils. The objective of this study is to evaluate the effect of low-rate fertilizer treatments with AVAIL® on dryland small grain yield on calcium-rich, eroded hillslopes in a fallow-wheat crop rotation. Two experiments were conducted to determine treatment effects on yield and grain quality for (1) above-ground dispersed (broadcast) application of monoammonium phosphate (MAP; 52% P2O5 content) fertilizer in the spring (2017), and (2) fall application of MAP incorporated with the seed (banded) at planting (2018). Fertilizer treatments were the recommended rate (60 lbs/ac) or one-half the recommended rate (30 lbs/ac) for dryland small grain, with or without AVAIL® (four treatments), replicated four times in a strip-block design for the 2017 experiment and replicated 3 times in a randomized complete block design for the 2018 experiment. Experimental blocks were assigned to hillslope erosional severity groups. The erosional severity groups were v designated (non-eroded, slightly eroded, highly eroded, and depositional slope segments). Hillslope segmentation allowed for correlations between calcium carbonate, organic matter, and yield levels across treatments. Results from the broadcast study indicate that there was no yield advantage of any treatment at any level of erosional severity, saving a grower $20.30/acre by applying 30 lbs/acre of MAP. However, 30 lbs/acre of MAP with AVAIL® showed similar yield to 60 lbs/acre of MAP without AVAIL®, potentially saving a grower $6.42/acre over standard growing practices. The incorporated study also indicated that there was no reliable yield advantage of any fertilizer treatment at any level of erosional severity, saving a grower $15.37/acre by applying 30 lbs/acre of MAP. Neither treatment with AVAIL had greater yield or profit than those without AVAIL. Profit for the 60 lbs/acre of MAP treatment narrowly outperformed 30 lbs/acre of MAP by $1.73/acre, indicating that growers may be able to reduce phosphorus use under dryland growing conditions with optimal fertilizer placement.

nitrogen has commonly been a deficient element in the cultivated soils of the world since the beginning of agriculture. The general acceptance of the practice of using manures as a means of increasing plant growth, as shown by the records of ancient civilizations, attest to this fact. Since the time of von Liebig there has been an increasing awareness of the importance of this deficiency in soils. As a result of a better understanding of the problem and the increasing availability of commercial forms of nitrogen, a rapid increase in the use of nitrogen fertilizers has taken place in the last few decades. this increasing use of commercial forms of nitrogen is accompanied by the need for more information concerning the proper use of these materials in order to accomplish the greatest benefit. For example, with the advent of increasing use of ammonium fertilizer to improve soil productivity, there has arisen a possibility of lengthening the period from the date of the fertilizer application to the time of utilization by the crop. this advanced application, especially in the fall of the year, has many advantages and is widely advocated. The following questions need to be answered in connection with efficiency of such a practice: Will the ammonium form of nitrogen remain unoxidized in the soil over the winter months? Could it be only partially oxidized and result in an accumulation of nitrites that may cause toxicity or be lost from the soil in gaseous forms such as nitrous oxide? What are the chance for significant losses by volatilization before it is oxidized? How does the amount of moisture and the prevailing temperature affect these transformations? The study reported here is an endeavor to contribute to more complete answers to some of these questions. Although much research has been conducted relating to the effects of moisture or temperature on nitrogen transformations in the soil, more information is needed covering greater variations in the moisture and temperature levels along with the interactions of these. Accordingly, experiments were conducted under carefully controlled conditions to measure the changes occurring in the inorganic soil nitrogen from an applied ammonium source, at various moisture and temperature levels.