The effects of irrigation-induced salinity and/or sodicity on sugarcane yield, and two growth parameters, namely stalk height and number of nodes per stalk , were investigated on a sugarcane estate in the Zimbabwean lowveld. The effects of soil salinity and/or sodicity on the size, activity and metabolic efficiency of the soil microbial community was also studied. Furrow-irrigated fields which had a gradient in soil salinity and/or sodicity which increased from the upper to lower ends of the fields were selected for this study. This gradient was recognized by decreasing sugarcane growth down from the upper to the lower ends and the appearance of salt on the soil surface at the lower ends of fields. Sugarcane growth was classified as either dead, poor, satisfactory or good; and soil samples (0-0 .15 m, 0.15-0 .3 m, 0.3-0 .6 m and 0.6-0.9 m) were taken from each of these areas. Soils from under adjacent areas of undisturbed veld were also sampled. Sugarcane growth and yields in micro-plots of the various areas of the fields were measured. Foliar samples of sugarcane were taken at 22 weeks of age and analysed for nutrient content. Soil salinity and sodicity were quantified by measuring pH(water), electrical conductivity (ECe) and cation content of saturation paste extracts and the exchangeable cation content. From this information, the sodium adsorption ratio (SARe)and exchangeable sodium percentage (ESP) were also calculated. The calcareous, vertic soils in the study area under undisturbed veld were found to have high pH values (8 to 9.5), very high exchangeable Ca and Mg concentrations and there was evidence of accumulation of soluble salts in the surface 0.15 m. Under sugarcane production, irrigation induced salinity and sodicity had developed. Under poor and dead sugarcane, high values for ECe, SARe, and ESP were generally encountered in the surface 0-0 .3 m of the profile. In addition, the pH values under sugarcane were often between 9 and 10 particularly in profiles where sugarcane grew poorly or had died. As expected, pH was positively related to ESP and SARe, but negatively related to ECe. Measurements of aggregate stability by wet sieving, the Emerson dispersion test and the Loveday dispersion score all showed that soils from the study sited tended to disperse and that dispersion was most apparent where high ESP and SARe values occurred in association with elevated pH values and relatively low ECe values. These measurements confirmed observations at the sites of low infiltration rates and restricted drainage particularly on the lower ends of fields where sugarcane had died. In addition to the above measurements it was also observed that there was a rise in the watertable under furrow irrigation and that the watertable was nearest to the surface at the lower ends of the fields. In some cases the watertable was observed to be only 0.2 to 0.3 m from the surface. Thus, death of roots due to anaerobic conditions could be occurring to a greater extent at the lower ends of the fields. Another consequence of the high watertable was that these vertic soils were observed to remain in a permanently swollen state. This limits air and water movement in the soil profile as such soils need to be allowed to dry out and crack regularly so that macroporosity can be restored. Sugarcane yield, stalk height and number of nodes per stalk were not significantly related to ECe. Sugarcane yields were, however, significantly correlated with ESP and pH while stalk height and number of nodes were negatively correlated with ESP, SARe and pH. These results suggested that sodicity was a more limiting factor for sugarcane growth than salinity. Foliar analysis of leaf tissue did not reveal substantial differences in macro- or micro-nutrient content between good and poorly-growing sugarcane. It was concluded that the gradient of decreasing sugarcane growth down the furrow-irrigated fields, with crop death at the lower ends, was the result of a combination of factors. That is, the watertable had risen due to over-irrigation and it was nearer the surface at the lower ends of the fields. Due to capillary rise of salts, this resulted in sodic and sometimes saline-sodic conditions in the surface soil. These conditions could limit plant growth through ion toxicities, plant water stress and inhibition of root growth and function and physiological processes. These would be induced by the high pH and high salt, Na and HC03- concentrations in soil solution. Poor physical conditions associated with sodicity and the continually swollen state of the soils presumably limited infiltration and aeration in the surface soil, and probably restricted root growth. In addition, it is likely that the high watertable limited effective crop rooting depth to about 0.2 m at the lower ends of the fields. The net result was that sugarcane died at the lower ends. A negative effect of soil salinity and/or sodicity was also observed on the soil microbial population. Significant negative correlations were obtained with ECe SARe and ESP with microbial biomass C and microbial activity (as measured by FDA hydrolytic activity or arginine ammonification rate). The activity of enzymes involved in C (P-glucosidase), P (phosphatase) and S (arylsulfatase) mineralization and potential nitrogen mineralization (as determined by aerobic incubation) were also negatively correlated with these factors, with the exception of arylsulfatase activity and ESP. All the above mentioned microbial population measures were also positively correlated with soil organic C content, besides potential nitrogen mineralization. The metabolic quotient, which provides an indication of stress and efficiency of the microbial community, increased considerably with increasing salinity and sodicity and decreased with soil organic C. Thus, increasing salinity and/or sodicity resulted in a smaller, more stressed, less efficient microbial community, while the turnover rate and cycling of C, N, P and S also decreased. It was concluded that salt affected soil not only causes a decline in sugarcane yield through raising the concentration of soluble salts in soil solution, but also has a detrimental effect on microbial activity and on mineralization of soil organic C, N, Sand P. / Thesis (M.Sc.)-University of Natal, Pietermaritzburg, 2001.

Studies were carried out in a lowland evergreen rain forest (LERF), on an ultisol, in the 'Reserva da Campina', 45 km north of Manaus, and in two facies of the highly distinct formation called heath forest, on spodosols. The spodosols had a layer of mor humus of thickness varying from nil in some parts in the smaller facies of heath forest (SHF) to 35 cm in the taller facies (THF). The overall aim was to investigate the forest soil biota and its role in nutrient turnover by comparing the SHF, THF and LERF. Microbial biomass, soil respiration and nitrogen transformation rates were measured in the three forest types in both wet and dry seasons. Field and laboratory fertilization experiments were made to investigate potential limiting nutrients for microorganisms and plants. The role of fine roots in decomposition and litter animal colonization was assessed in litter bag studies. SHF soils have a small microbial population with no net nitrification in any season. THF soils showed a variable microbial population adapted to high acidity, which immobilises nitrogen during the wet season, but which allows a net release during the dry season. LERF showed the most diverse population which causes mineralization and nitrification in both seasons. A bioassay with nutrient addition showed that the low pH, and nitrogen and sulphur supply were likely to be limiting nitrogen dynamics in all forest types, but especially in THF and LERF. The ingrowth bags showed that despite the lower values of fine root growth in the SHF (particularly when the white sand of the spodosol was used as the substrate), the roots showed in all plots an increased production with added calcium as carbonate or sulphate. In the decomposition bioassay to evaluate the role of roots in the nutrient turnover it was shown that in all forest types there was no effect of roots on the mass loss of Clitoria leaves but there was a significant effect on concentrations of some nutrients. In general, roots contributed to the accumulation of aluminium and iron and to a faster release and uptake of calcium, magnesium and zinc. A survey of the mycorrhizal associations in all forest types showed that both VAM and ECM fungi with some unknown VAM fungal species are common. VAM and ECM adaptation to low pH and high phenolic compounds in the soils may be important in the maintenance of these ecosystems.

Oil palm is the largest national crop produced in Papua New Guinea. It is grown on over 80,000 ha of young volcanic soils in five Provinces, employs over 12,000 workers and uses >12,000 tonnes of fertiliser to offset nitrogen deficiency which is the most limiting factor to production. Oil palms strip out 160 - 200 kg N ha-1 yr-1 from the soil. Nitrogen fertilisers account for 60-70 % of all variable production costs but 40-60 % of applied fertiliser cannot be accounted for. Few studies have investigated the amounts of nitrogen lost via leaching, denitrification, volatilisation or as surface runoff in tropical soils and none have been done in Papua New Guinea. Oil palm soils typically have extremely high infiltrabilities (80-8,500 mm hr-1) and receive high annual rainfall which throughfall makes spatially non-uniform. The objective of this study was to assess and quantify nitrogen losses and suggest strategies that might assist in reducing them and their impact on the environment. The modest facilities available at the two research sites, West New Britain (Dami) and Oro (Sangara) Provinces, meant that no analytical work could be done on-site, so simple but appropriate methods were used to evaluate losses, with samples collected, preserved and sent off-shore for analysis. Large four-palm plots were used to evaluate runoff; a gas trap was used to collect evolved nitrous oxide, and lysimeters, suction cups and finally an in situ destructive soil sampling procedure were all used to assess leaching losses and the rate of nitrification of ammonium fertiliser. Results suggest that under the extreme total annual rainfall at Dami (3,500-4,000 mm) and to a lesser extent at Sangara (2,500-3,000 mm), leaching is the dominant loss pathway, with the rate of loss depending, to some extent, on the rate of nitrate formation and the retentivity of the soil for ammonium, but mainly on the rate at which drainage water is generated. A leaching model was developed that indicated that the average residence time of nitrogen fertiliser in the root zone (0-50 cm) varied from 21 days in February, at Dami, to 190 days in May, at Sangara.

Diss. (sammanfattning) Uppsala : Sveriges lantbruksuniv., 2003. / Härtill 4 uppsatser.

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Made available in DSpace on 2014-07-29T16:24:17Z (GMT). No. of bitstreams: 1 Dissertacao Glaucilene Duarte Carvalho.pdf: 1045002 bytes, checksum: 3cead1a1cea2b6c0d5785f15e2938316 (MD5) Previous issue date: 2011-02-15 / In wetland soils are countless electrochemical changes, among the most influenced by anaerobic conditions is nitrogen. The rice crop also determine changes in the process, either by the nutrient uptake or by changes in the rhizosphere. The nitrogen can guarantee high yields of rice, however, due to the inadequate use of nitrogen can have nitrous oxide, which is a greenhouse gas. In this context, the research aimed to determine the effects of nitrogen fertilizer in flooded lowland soils in soil chemistry and soil solution on the plants and the emission of nitrous oxide. The experiment was conducted in pots at Embrapa Rice and Beans. The treatments consisted of two rice genotypes (BRS Tropical and BRA 051130) and three nitrogen (0, 150 and 300 mg N kg-1 soil). The experimental design was randomized blocks with split plots. The flooding of the vessels took place on the fifteenth day after planting. The collection solution was given 1, 3, 7, 14, 28, 39, 59, 67, 102 days after flooding. The collection system consisted of a perforated plastic pipe and secured in the vessel walls, being closed at the ends. The solution was suctioned through a syringe and then analyzed on Ca, Mg, K, P, Fe, Mn, NO3 -, NH4 +, pH and Eh (directly to the pots). After the experiment was made at the soil sampling vessel, comprising all the other treatments being performed analysis of Ca, Mg, K, P and soil pH. The yield components studied were: plant height, tiller number, panicle number per plant, panicle length, spikelet sterility, dry weight of 1000 grains, shoot dry weight, root dry mass, grain yield, root length, grain harvest index, the contribution of the shoot dry weight total contribution of root dry weight total. The method of collection of nitrous oxide was a closed chamber in PVC material. Collections were undertaken throughout the rice cycle and N2O concentration was measured by reading in a gas chromatograph. The results were subjected to analysis of variance, treatment means compared by Tukey test. The pH, exchangeable Ca, Mg, K and P in soil increased after the implementation of the experiment. The values of Eh in soil solution decreased with time of flooding and consequently the pH increased. The concentration of Ca and Mg in soil solution increased with time of flooding and the K, Mn, NO3 -, NH4 + declined over the period. The rice genotypes showed differences in dry weight of 1000 grains. The dry weight of shoots showed responses to nitrogen fertilization, since the height of the trees showed responses to genotypes and N levels The total emission of N2O showed differences in nitrogen use and for the rice genotypes. We observed that the genotype BRA 051130 showed significantly higher total emission in relation to the treatment without plants. / Em solos inundados inúmeras são as alterações eletroquímicas que ocorrem, dentre os elementos mais influenciados pelas condições de anaerobiose está o nitrogênio. O cultivo de arroz irrigado também determinará alterações no processo, quer pela absorção de nutriente quer por modificações da rizosfera. A adubação nitrogenada pode garantir altas produtividades do arroz, porém, em consequência do uso inadequado do nitrogênio pode-se ter emissões de óxido nitroso, que é um gás de efeito estufa. Nesse contexto, a pesquisa teve o objetivo de determinar os efeitos da adubação nitrogenada em solos de várzeas inundados na química do solo e da solução do solo, na planta e na emissão de óxido nitroso. O experimento foi realizado em vasos na Embrapa Arroz e Feijão. Os tratamentos consistiam de dois genótipos de arroz irrigado (BRS Tropical e BRA 051130) e de três doses de nitrogênio (0, 150 e 300 mg de N kg-1 de solo). O delineamento experimental utilizado foi blocos ao acaso com parcelas subdivididas. A inundação dos vasos se deu aos quinze dias após o plantio. A coleta de solução se deu 1, 3, 7, 14, 28, 39, 59, 67, 102 dias após a inundação. O sistema de coleta consistiu em uma mangueira de plástico perfurada e fixada nas paredes dos vasos, sendo fechadas nas extremidades. A solução foi succionada por meio de uma seringa e depois realizadas as determinações de Ca, Mg, K, P, Fe, Mn, NO3 -, NH4 +, pH e Eh (diretamente nos vasos). Ao término do experimento fez-se a amostragem do solo dos vasos, contemplando todos os tratamentos; sendo realizada análises de Ca, Mg, K, P e pH do solo. Os componentes de produção estudados foram: altura de plantas, número de perfilhos, número de panículas por planta, comprimento de panículas, esterilidade de espiguetas, massa seca de 1000 grãos, massa seca da parte aérea, massa seca da raiz, produtividade de grãos, comprimento da raiz, índice de colheita de grãos, contribuição da parte aérea na massa seca total, contribuição da raiz na massa seca total. O método de coleta de óxido nitroso foi o de câmara fechada em material de PVC. Realizaram-se coletas ao longo de todo ciclo do arroz e a concentração de N2O foi obtida por meio da leitura em cromatógrafo gasoso. Os resultados foram submetidos à análise de variância , sendo as médias dos tratamentos comparadas pelo teste de Tukey. O pH, os teores de Ca, Mg, K e P no solo aumentaram após a implantação do experimento. Os valores de Eh na solução do solo diminuíram com o tempo de inundação e, consequentemente o pH aumentou. A concentração de Ca e Mg aumentaram na solução do solo com o tempo de inundação e os teores de K, Mn, NO3 -, NH4 + reduziram ao longo do período. Os genótipos de arroz irrigado apresentaram diferenças em relação a massa seca de 1000 grãos. A massa seca da parte aérea apresentou respostas a adubação nitrogenada, já a altura de plantas apresentou respostas aos genótipos e à dose de N. A emissão total de N2O apresentou diferenças quanto ao uso de nitrogênio e em relação aos genótipos de arroz irrigado. Sendo observado que o genótipo BRA 051130 apresentou emissão total significativamente maior em relação ao tratamento sem planta.

A preocupação com a contaminação por metais reflete na busca de metodologias de recuperação de solos. O objetivo deste trabalho foi compreender os mecanismos de formação e oxidação dos sulfetos em solos e propor uma metodologia de imobilização de metais pela formação de sulfeto insolúvel e posterior fitoextração. Três experimentos foram conduzidos em solos contaminados com Cd e Zn. O primeiro teve como objetivo definir a concentração de (NH4)2S necessária para a formação dos sulfetos metálicos. Os resultados confirmam que a adição de sulfeto reduz a disponibilidade de Cd e Zn em Argissolos Vermelho-Amarelos distróficos e que concentrações de sulfetos superiores a 30 e 60 mmol kg-1, respectivamente para Cd e Zn, não melhora a capacidade de imobilização dos metais. O segundo experimento objetivou avaliar a influência da matéria orgânica, pH, tempo e ambiente na imobilização de Cd e Zn associado ao sulfeto. Foi demonstrado que a adição de matéria orgânica reduz a concentração de Cd solúvel e mantém o pH em faixa adequada às plantas. Para o Zn, a matéria orgânica não apresentou efeito significativo, prevalecendo o efeito do sulfeto. O aumento do pH, através da adição de carbonatos aumenta a imobilização do Cd e Zn em presença de sulfeto, influenciado pela formação dos respectivos hidróxidos. A exposição dos sulfetos metálicos a um ambiente oxidante reduz a imobilização de Cd e Zn devido à sua oxidação e consequente dissociação molecular. O terceiro experimento, desenvolvido em casa de vegetação, avaliou a disponibilidade de Cd e Zn e sua toxidez em Phaseolus vulgaris L. (feijão), utilizando a melhor dose de sulfeto com adição de matéria orgânica para obter maior eficiência na imobilização. A produção de massa seca da planta foi superior em solos que não continham sulfeto, o que indica fitotoxicidade. Concluímos que soluções de sulfeto podem ser utilizadas para imobilização temporária de Cd e Zn em solos contaminados, entretanto sua aplicação combinada à fitorremediação necessita de maiores estudos / The development of remediation of soil degraded areas methodologies reflects the concern with the metal contamination. The aim of this work was to understand the formation mechanisms and oxidation of sulfides in soils and propose a metal immobilization procedure by precipitation an insoluble sulfide and subsequent phytoextraction. Three experiments were conducted in contaminated soils with Cd and Zn. The first aimed to determine the (NH4)2S concentration necessary for the metallic sulfide formation. The results confirm that the sulfide addition reduces the Cd and Zn available in red-yellow dystrophic Argisoil and sulfide concentration above 30 and 60 mmol kg-1, respectively for Cd and Zn, not improve the metals immobilizations. The second experiment evaluated the organic matter, pH, time and atmosphere influence in the Cd- and Zn-sulfide immobilization. The addition of organic matter reduces the concentration of soluble Cd and maintaining the pH in adequate range for plants. For Zn, organic matter didn\'t show significant effect, prevailing the sulfide effect. The increase in pH by carbonates addition increases the Cd and Zn immobilizations in the sulfide presence. The exposure of metallic sulfide to an oxidizing atmosphere reduces Cd and Zn immobilization. The third experiment, developed in greenhouse, evaluated the Cd e Zn toxicity in Phaseolus vulgaris L. (bean) by using the best sulfide dose and addition of organic matter. The dry matter production was higher in soils without sulfide, indication phytotoxicity. We conclude that sulfide solutions can be used for Cd and Zn temporary immobilization in contaminated soils, however the application combined with phytoremediation needs further studies

Com o objetivo de avaliar o uso de extratores de soluções do solo no auxílio ao manejo da fertirrigação e no controle da salinidade em solo cultivado com melão rendilhado, conduziu-se um estudo em ambiente protegido na área experimental do Departamento de Engenharia Rural da ESALQ/USP, localizado no município de Piracicaba, SP. Os tratamentos foram compostos da combinação de dois fatores: 6 níveis de salinidade inicial do solo (S1 = 1,0; S2 = 2,0; S3 = 3,0; S4 = 4,0; S5 = 5,0 e S6 = 6,0 dS m-1) e dois manejos de fertirrigação: tradicional e com controle da condutividade elétrica da solução do solo. O delineamento estatístico adotado foi o de blocos casualizados completos com 4 repetições, sendo os fatores estudados arranjados em um esquema fatorial de 6 x 2. A salinização inicial do solo se procedeu por meio da aplicação de soluções salinas preparadas a partir de fertilizantes, sendo que a quantidade de sais a ser adicionada foi determinada tomando por base uma curva de salinização artificial obtida previamente em laboratório. A condutividade elétrica da solução foi medida após o término de cada evento de irrigação, utilizando-se extratores com cápsulas porosas. Os resultados revelam que as produções total e comercial, além do peso médio total dos frutos foram significativamente reduzidos com o incremento dos níveis de salinidade do solo Os efeitos da salinidade do solo sobre a altura e o diâmetro das plantas foram mais severos durante o desenvolvimento vegetativo inicial do que no início da frutificação, o que sugere uma possível adaptação das plantas ao estresse salino ao longo do tempo. Embora não tenha sido possível se detectar diferenças expressivas causadas pelos dois tipos de manejo da fertirrigação no desenvolvimento ou na produção da cultura, o uso dos extratores de solução permitiu auxiliar no manejo da fertirrigação, mantendo os níveis desejados de salinidade da solução do solo ao longo do tempo. / A study was carried out under greenhouse conditions, at the experimental area of the Department of Rural Engineering of “Escola Superior de Agricultura Luiz de Queiroz-USP”, Piracicaba, São Paulo State, Brazil, with the aim of evaluating ceramic cup samplers used to facilitate fertirrigation management and soil salinity control on a netmelon crop, was carried out The treatments comsisted of two combination factors: six level of initial soil salinity (S1 = 1.0, S2 = 2.0, S3 = 3.0, S4 = 4.0, S5 = 5.0 and S6 = 6.0 dS m-1) and two fertirrigation managements: the traditional and the control of eletrical conductivity of soil solucion. The statiscal test was in randomized blocks, with four replications, arranged in 6 x 2 factorial design. The initial soil salinity value was obtained by appling saline solutions of fertilizer salts using an artificial soil salinization curve obtained previously in laboratory. The electrical conductivity in soil solucion was measured after each irrigation using ceramic cup samplers. Results showed that both total and marketable fruit yield and total weight per fruit were significantly reduced by increase in soil salinity level. The soil salinity effects on plants height and stem diameter were more severe during early vegetative growth than in the beginning of fruit set. This suggests a possible plant adaptation to saline stress along the time. Although no differences were observed in case fertirrigation management treatments on plants development or yield, however the use of solution extractors helped in fertirrigation management because them permitted to keep soil solution salinity at desired level.

In Peru, nearly 32 million people rely heavily on human-made coastal irrigation agricultural hubs that rely on water from melting glaciers, snowpack, and rain transported by rivers and canals from high in the Andes. However, Peru’s water resources are in a vulnerable state as climate change has shifted rainfall patterns causing glacier retreat affecting nearly the loss of one-third of the glaciers. In recent decades, an increase and expansion of irrigation projects in Peru require agriculture practices to consider environmental impacts directly. Now is the time to explore the sustainability of the desert agroecosystems and understand how different water management practices influence the supporting soil’s health so decision-makers can plan for future change in water resources and any feedbacks to the productivity of the soils. Over the past 40 years, Peru has led some of the largest scale water management projects on earth to convert infertile coastal desert soils into irrigated agricultural land. Still, these efforts can come at a severe local cost with impacts to groundwater quality, salination of the soil, toxic concentrations of trace metals due to evaporation, and overuse of fertilizer and pesticides. This thesis presents a study to assess how drip irrigation impacts desert soil chemistry within one of Peru’s desert irrigation projects in Arequipa’s southern district. We explored a chronosequence of drip irrigation in vineyards of 9-, 16- and 35- years. Results showed that both soil carbon and salinity accumulated progressively over time but that spatial accumulation patterns were influenced by proximity to the irrigation drip line. By 35 years, salinity levels exceeded what would be tolerances for most crops. Trace metals, such as Mn, Zn, and Ni, increased with time under drip irrigation and have significant relationships with Fe, present in the highest concentrations, seemingly controlling the patterns due to co-precipitation. However, no trace metals were found in quantities that would exceed Peru’s limits for agricultural soils. While drip irrigation is considered a water conservation strategy and widely promoted in the region over other irrigation techniques like high water volume furrow irrigation, its use may accelerate localized negative impacts to surface soil health. These progressive changes highlight the need for effective monitoring and salinity mitigation strategies in the region. This project is part of the bilateral technical program between Purdue University and Universidad Nacional San Agustín (UNSA) called the Arequipa Nexus Institute for Food, Water, Energy, and the Environment.