Coordenação de Aperfeiçoamento de Pessoal de Nível Superior / Petroleum exploration, an activity that generates economic benefits, can also bring environmental impacts, one of which associated with large quantities of produced water discharged into aquatic environments. A particular concern is that these discharges contain significant amount toxic compounds including benzene, toluene, ethylbenzene and isomers of xylene (BTEX). One option to be employed to minimize the concentrations of these compounds entering the environment is to treat the water prior to discharge. The present work therefore investigates the potential of peat and angico sawdust to remove BTEX from produced water. Samples of produced water was collected from the Bonsucesso treatment station, operated by Petrobras in of Carmópolis City, Brazil. In batch experiments, the removal capacity of the peat was 32.4, 50.0, 63.0, 67.8 and 61.8% for benzene, toluene, ethylbenzene, m,p-xylene and oxylene, respectively. Comparing with removal capacities of angico sawdust of 20.2, 36.4, 52.8, 57.8 and 53.7% for these compounds, respectively, peat has show a superior performance of removal. Identification and quantification of BTEX was done by gas chromatography. After optimization, accuracy exceeding 90 %, precision better than 6 %, linear determination coefficient (r2) of 0.998, and limits of detection and quantification of 0.09-0.18 μg L-1 and 0.27-0.35 μg L-1, respectively. This work has demonstrated considerable potential of alternative materials for efficient removal of organic compounds from aqueous media. / A exploração de petróleo, uma atividade que gera desenvolvimento econômico, traz consigo uma parcela de agressão ao meio ambiente. Um exemplo disso é o volume de água produzida descartado diariamente em ambientes aquáticos. Esse descarte se torna preocupante devido à presença de inúmeros compostos tóxicos, dentre eles Benzeno, Tolueno, Etilbenzeno e isômeros de Xilenos. Uma solução para minimizar esses efeitos seria tratá-la antes do descarte. No presente trabalho foi avaliado o potencial de adsorção em batelada utilizando turfa e serragem de angico como adsorventes na remoção de BTEX em água produzida. A amostra de água produzida foi coletada na cidade de Carmópolis/SE. A capacidade de remoção da turfa foi de 32,4, 50,0, 63,0, 67,8 e 61,8% para Benzeno, Tolueno, Etilbenzeno, m,p-Xileno e o-Xileno, respectivamente. Quando comparada com a serragem de angico, para o qual foi determinado uma remoção de 20,2, 36,4, 52,8, 57,8 e 53,7% para Benzeno, Tolueno, Etilbenzeno, m,p-Xileno e o-Xileno, respectivamente, ficou evidenciado uma maior capacidade de remoção da turfa. A identificação e quantificação dos BTEX foram feitas por cromatografia gasosa. A otimização e validação do método cromatográfico apresenta bons resultados, com exatidão acima de 90%, precisão abaixo de 6%, linearidade com coeficiente de determinação (r2) acima de 0,998, limite de detecção entre 0,09 - 0,18 μg L-1 e limite de quantificação entre 0,27 - 0,35 μg L-1. Este trabalho demonstrou alto potencial de materiais alternativos na remoção de compostos orgânicos em meio aquoso.

Nesta pesquisa foram estudadas morfologias e posições do relevo que apresentam solos e depósitos com regimes hídricos caracterizados pela saturação temporária ou permanente, tendo os seguintes objetivos: (i) caracterização dos solos e depósitos presentes no setor inferior de vertentes e em fundos de vale, incluindo planícies fluviais, com ênfase em suas propriedades hidromórficas; (ii) identificação de graus de hidromorfia nos solos e depósitos desses setores e morfologias, e representação de sua variabilidade espacial; (iii) elaboração de proposições a respeito do regime de saturação hídrica nos setores estudados e de sua relação com os graus de hidromorfia identificados; (iv) elaboração de proposições sobre tendências espaciais hidrodinâmicas associadas à inundação fluvial nas áreas de planície. Sob o aspecto metodológico, a pesquisa foi desenvolvida de acordo com os princípios da abordagem geossistêmica, apresentando uma análise integrada que buscou identificar as inter-relações entre as variáveis pesquisadas. Para tal estudo, foram selecionados dois perfis transversais na Alta Bacia Hidrográfica do Rio Cotia, que abrangeram o setor inferior de vertentes e fundos de vale, um deles com planície fluvial. Ao longo desses perfis transversais foram realizados os seguintes levantamentos e procedimentos: (i) levantamento morfométrico e construção de gráficos dos perfis; (ii) descrição dos atributos morfológicos dos solos e depósitos; (iii) monitoramento dos níveis dágua do lençol freático ou lençol suspenso nos pontos de descrição. A caracterização e análise detalhadas das propriedades hidromórficas revelaram gradações de intensidade nas mesmas, e, a partir dessa base, desenvolveu-se uma proposta para classificação dos solos e depósitos segundo graus de hidromorfia. Foram construídas representações gráficas bidimensionais que ilustraram a sucessão vertical e lateral de horizontes pedogenéticos e camadas com diferentes graus de hidromorfia ao longo dos setores e morfologias estudadas. Desta maneira, foram identificadas tendências gerais no que se refere à distribuição espacial dos graus de hidromorfia e à relação desses graus com o regime de saturação hídrica. Um dos padrões identificados consistiu no aumento do grau de hidromorfia dos perfis verticais de solos e depósitos com o aumento da profundidade, que está associado a um maior tempo de duração das condições de saturação hídrica nos horizontes mais profundos. Também foram observadas diferenças significativas na intensidade das propriedades hidromórficas das vertentes, quando comparadas às áreas de fundos de vale, incluindo a planície fluvial. Neste sentido, foram identificados graus de hidromorfia mais baixos nos horizontes A e B dos pontos localizados nas vertentes, e graus mais elevados nos horizontes A e B dos pontos localizados nos fundos de vale. Essas diferenças na ocorrência dos graus de hidromorfia foram atribuídas a distintos regimes de saturação hídrica, sendo que, de maneira geral, os horizontes pedogenéticos e as camadas com graus de hidromorfia elevados estão sujeitos a condições de saturação hídrica de maior duração ou permanentes, quando comparados àqueles que possuem graus de hidromorfia mais baixos, nos quais os eventos de saturação hídrica tem menor duração e/ou ocorrem com menor frequência. Com relação às proposições referentes à inundação fluvial na planície estudada, foram identificadas morfologias que recebem preferencialmente os fluxos fluviais da inundação e apresentam taxas de deposição mais elevadas, e setores com taxas de deposição mais baixas nos quais a inundação é menos frequente e há predomínio da deposição de sedimentos finos. / In this research we studied morphologies and relief positions with soils and deposits with moisture regimes characterized by temporary or permanent water saturation, with the following objectives: (i) characterization of soils and deposits located in lower slope sectors and valley bottoms, with an emphasis on their hydromorphic properties; (ii) identification of degrees of hydromorphy in the soils and deposits of these sectors and morphologies, and representation of their spatial variability; (iii) development of propositions about the regime of water saturation in the studied areas and its relationship with the degrees of hydromorphy; (iv) development of propositions about the hydrodynamics of floods in the studied floodplain. Regarding the methodological aspect, the research was conducted according to the principles of the geosystemic approach, presenting an integrated analysis which considered the inter-relations among the studied variables. For this study, we selected two cross profiles in the Cotia Drainage Basin, comprising lower slope sectors and valley bottoms, including a floodplain. Along these cross profiles, the following surveys were conducted: (i) topographic survey and construction of cross section graphics; (ii) description of the morphological attributes of soils and deposits, including detailed description of their hydromorphic properties; (iii) monitoring the water levels of the water table and perched water tables in the sites of description. The detailed characterization and analysis of the hydromorphic properties revealed gradations of intensity in them, and, based primarily on this, we developed a proposal for classification the soils and deposits of the study area according to degrees of hydromorphy. We built two-dimensional graphical representations which illustrated vertical and lateral successions of pedogenetic horizons or layers with different degrees of hydromorphy. Thus, general trends were identified in respect to the spatial distribution of the degrees of hydromorphy and in respect to its relationship with the regime of water saturation. One of the patterns identified consisted in the increase of the degree of hydromorphy in the soil profiles with increasing depth, associated with a longer duration of water saturation conditions in the deeper horizons. It were also observed significant differences in the intensity of the hydromorphic properties of the slopes, when compared to the valley bottom areas, including the floodplain. In this regard, lower degrees of hydromorphy were identified in the A and B horizons in the slope sectors, and higher degrees in the A and B horizons in the valley bottom areas. Such differences in the degree of hydromorphy were ascribed to distinct regimes of water saturation, considering that, in general, the horizons and layers with higher degrees of hydromorphy are subject to water saturation conditions of longer duration, when compared to those classified according to lower degrees of hydromorphy, in which the water saturation events have shorter duration and/or have lower frequency. Concerning the propositions about the hydrodynamics of floods in the studied floodplain, we identified morphologies that preferentially receive the overflowing river flows and have higher deposition rates, and sectors with lower deposition rates, where flooding is less frequent and there is a predominance of fine sediments deposition.

Peat moorlands represent a nationally significant carbon store. Wildfires in peat moorlands release CO2 into the atmosphere, reducing the carbon store and burn into the seed bank preventing vegetation recovery. Burned areas of bare peat remain, known as ‘burn scars’ which are eroded by freeze thaw and desiccation, then weathered by precipitation and wind to cause discolouration of the water supply. A technique for the systematic monitoring of peat moorland burn scars is essential for informing land management and moorland restoration. Satellite data enables peat moorland burn scars to be monitored at the landscape scale for operational services e.g. European Forest Fire Information System (EFFIS). However, in the UK cloud is highly problematic for optical satellites and thermal data provides only a short window of opportunity for active fire detection. This thesis provides a unique line of enquiry by exploring the potential of Synthetic Aperture Radar (SAR) intensity and Interferometric Synthetic Aperture Radar (InSAR) coherence for burn scar characterisation and persistence, using a multi-temporal and multi-sensor approach for degraded peat moorland. The Peak District National Park (PDNP) was selected because it is a marginal moorland environment, which experiences high rates of peat erosion and will experience more wildfires, based on future projections of increased temperature, due to global warming. Initial SAR intensity results for the Bleaklow 2003 burn scar showed a clear post-fire increase of 7 dB for burned peat bog when acquired under wet conditions. Post-fire, dry − wet InSAR pairs were characterised by vegetation removal caused by combustion within the burn scar area, whereas wet − wet InSAR pairs characterised the burn scar, but also degraded peat moorland caused by previous wildfires blurring the new burn scar perimeter. Intensity differed significantly with slope for the PDNP 2003 wildfires, reducing the effectiveness of the technique for characterising burn scars on slopes facing away from the sensor, although these wildfires showed no significant difference on coherence for the inland bare ground class. When using coherence as a burn scar discriminator, this research found that it is essential to acquire InSAR pairs immediately post-fire with B⊥ < 550 m. Using a combination of intensity and coherence data a multi-difference colour composite was produced and an ISODATA classification applied. Results were reclassified to produce a burned area map with an overall map accuracy of 94% and Kappa Coefficient of 0.69 covering the Bleaklow and Kinder 2003 burn scars. Burn scars < 6 km2 provided a persistently higher burned area intensity signal for up to six months after the wildfire but only 2 − 3 months for coherence. The smaller Edale burn scar (0.10 km2) was characterised by 2 − 3 dB greater intensity for the burned area over a year after the wildfire. The Edale 2008 case study showed that L-band PALSAR data is less sensitive to characterising peat moorland burn scars compared to C-band data. This study therefore strongly recommends C-band data for peat moorland burn scar characterisation and monitoring. Future research will explore the new C-band Sentinel-1 data which offers improved spatial resolution and repeat-pass time.

Abstract Treatment wetlands (TW) constructed on natural wetlands potentially perform efficient purification of wastewater, but the longevity of TWs at northern latitudes is not well known. This thesis examined processes affecting nutrient and suspended solids (SS) retention in TWs during their lifetime. In total, 15 TWs were studied using water and peat quality and gas flux data for different TW life lengths, the longest period being 18 years. The TWs commonly retained nutrients and suspended solids efficiently, even after 18 years of wastewater loading. For nitrogen (N) removal, sedimentation, nitrification-denitrification and plant uptake were efficient processes in the wetlands studied. However, emissions of nitrous oxide (N2O) from TWs are not a major contributor to climate change due to the small total surface area of TWs. The significance of anaerobic ammonium oxidation (anammox) and other newly discovered nitrogen processes in TWs remains to be clarified. Phosphorus (P) adsorption capacity in TWs remained efficient over a 12-year study period, the process being continuous when surfaces for adsorption were available or freed up through alternating absorption/desorption/adsorption. Phosphorus accumulation by peat accretion was low, but has not been well assessed in northern TWs receiving nutrient-rich waters. Iron (Fe) and aluminium (Al) in peat extraction runoff and purified wastewater from sewage treatment plants were of great importance for precipitation of P in TWs. Filtration and sedimentation of organic humic substances with Fe- or Al-bound P were other probable P retention pathways. In peat extraction runoff, Fe was more significant than Al for P retention, but Fe-bound P is susceptible to desorption in anaerobic environments, whereas Al-bound P is more strongly retained. Suspended solids were generally retained well, although there was great variation in percentage retention in individual TWs in different years and different seasons. Changes in discharge affected SS transportation and retention. SS were retained by sedimentation, the rate of which was affected by particle size. It is plausible that smaller particles from old peat extraction areas where the extracted peat has a high humification degree erode more easily than poorly humified particles in surface peat. Weakened SS retention may also have been caused by development of preferential flow areas (PFA) in TWs, changes in sediment delivery characteristics and sampling involving too few samples to show SS transportation sufficiently accurately for estimating SS retention. Thus TWs are potentially ideal for purification of wastewater and can have high purification efficiency even after long-term use in northern regions. They are also more widely applicable as long as their limitations are understood. / Tiivistelmä Kosteikkopuhdistamot, jotka on rakennettu luonnonkosteikoille, voivat tehokkaasti vähentää erilaisten maankäyttömuotojen ja pistekuormituslähteiden vesistökuormitusta. Niiden käyttöikää pohjoisilla alueilla ei kuitenkaan tunneta hyvin. Tässä väitöskirjassa tarkastellaan kosteikkopuhdistamoissa tapahtuvia biologisia, kemiallisia ja fysikaalisia prosesseja, joilla on vaikutusta ravinteiden ja kiintoaineen pidättymiseen. Yhteensä 15 eri-ikäisen kosteikkopuhdistamon toimintaa tutkittiin veden ja turpeen laadun sekä kasvihuonekaasumittausten avulla. Näistä vanhinta kosteikkoa oli tutkimusta tehdessä käytetty 18 vuotta turvetuotannon valumavesien puhdistukseen. Tyypillisesti kosteikkopuhdistamot pidättivät ravinteita ja kiintoaineita tehokkaasti jopa 18 vuoden käytön jälkeen. Typenpoistossa sedimentaatio, nitrifikaatio-denitrifikaatio ja kasvien ravinteidenotto olivat tutkituilla kosteikoilla tehokkaita prosesseja. Kosteikkopuhdistamoiden typpioksiduulipäästöt (N2O) ilmaan eivät kuitenkaan ole merkittäviä ilmastonmuutoksen aiheuttajia, koska tällaisten kosteikkopuhdistamoiden kokonaispinta-ala on pieni. Anammox- (anaerobic ammonium oxidation) ja muiden viimeaikoina muissa tutkimuksissa havaittujen typpiprosessien merkitys kosteikoilla tulisi vielä selvittää. Fosforin adsorptiokyky kosteikkopuhdistamoilla pysyi tehokkaana 12 vuoden tutkimusjaksolla, koska niissä adsorptiopintoja oli joko vapaana tai niitä vapautui absorptio- ja desorptioprosessien seurauksena. Kosteikkopuhdistamolla fosforin kertyminen turpeen muodostuksessa arvioitiin vähäiseksi, tosin kertymistä ei ole tarkkaan määritetty pohjoisilla kosteikkopuhdistamoilla, joihin tulee ravinteikasta vettä. Turvetuotannon valumavesissä ja jätevedenpuhdistamoilta tulleissa vesissä orgaanisten humusaineiden rautaan ja alumiiniin sitoutuneen fosforin suodattuminen ja sedimentoituminen olivat muita todennäköisiä fosforin pidättymismekanismeja kosteikoilla. Turvetuotannon valumavesissä rauta oli alumiinia merkittävämpi tekijä fosforin pidättymisessä. Rautaan sitoutunut fosfori on kuitenkin altis desorptiolle hapettomissa olosuhteissa, kun taas alumiiniin sitoutunut fosfori pidättyy pysyvämmin. Kiintoaines pidättyi kosteikkopuhdistamoissa yleensä hyvin, vaikka pidättyneen aineen osuudessa kokonaiskuormituksesta oli suurta vaihtelua yksittäisissä kosteikkopuhdistamoissa eri vuosina ja eri vuodenaikoina. Muutokset virtaamissa vaikuttivat kiintoaineksen kulkeutumiseen ja pidättymiseen. Kiintoaines pidättyy sedimentaatiossa, jonka suuruuteen vaikuttaa kiintoaineen partikkelikoko. On todennäköistä, että vanhojen turvetuotantoalueiden korkean humusasteen pienikokoiset turvepartikkelit erodoituvat helpommin kuin pintaturpeen vähemmän hajonneet partikkelit. Heikentynyt kiintoaineen pidättyminen saattaa aiheutua myös kosteikkopuhdistamoiden oikovirtauksien kehittymisestä, muutoksista sedimentin kulkeutumistavoissa ja liian harvoista näytteenotoista, jolloin ei pystytä riittävän tarkasti arvioimaan kiintoaineksen pidättymistä. Kosteikkopuhdistamot voivat olla ideaalisia jätevesien puhdistamiseen ja ovat osoittaneet hyvää puhdistustehokkuutta myös pitkäaikaisessa käytössä pohjoisissa olosuhteissa. Siten ne ovat laajasti sovellettavissa, kunhan niiden käyttömahdollisuuksien rajoitteet on otettu huomioon.

Abstract Chemical treatment is considered best available technology for purification of peat extraction runoff in Finland, due to its capability to remove dissolved organic carbon (DOC), suspended solids and nutrients. However, lack of optimisation and adaptation of this method for purification of diffuse pollution sources, e.g., peat extraction runoff, has led to significant fluctuations in purification efficiency. This thesis evaluated the suitability of commercially available coagulants for the treatment of typically humic water. Inorganic (ferric sulphate, aluminium sulphate and a mixed product) and organic (polyDADMAC, polyamine, chitosan and tannin products) coagulants were studied. Investigations included assessment of required dosage and the influence of process parameters (pollutant concentration, mixing, water pH and temperature) on coagulant performance. In addition, the process conditions in existing treatment systems were examined in field experiments aimed at identifying possible factors affecting purification. Ferric sulphate (FS) was the most effective of the coagulants tested. It produced excellent flocs and achieved higher removal efficiency, particularly for DOC, than the other coagulants. However, the dosage required for FS was significantly higher than for e.g., polyDADMAC and chitosan. Moreover, samples treated with FS displayed high iron concentration and acidic pH. The organic polymers achieved satisfactory results, but further research is needed before they can become viable alternatives to metal salts. The quality of peat extraction runoff water was found to vary significantly. It was also observed that variations in DOC concentration, even for particulate rich samples, controlled coagulant dosage and, consequently, treatment efficiency. For inorganic coagulants, mixing provided during flocculation had a more significant influence on purification than mixing provided during coagulation. This is relevant hence in now existing treatment facilities no mixing is employed during flocculation. Based on the research conducted, suggestions were formulated for process optimisation aimed at reducing variations in purification efficiency, thus increasing the reliability of the method and reducing related environmental impacts. / Tiivistelmä Turvetuotannon valumavesien käsittelyssä yksi parhaista käyttökelpoisistatekniikoista on kemiallinen käsittely, koska se pystyy poistamaan valumavedestä liukoista orgaanista hiiltä (DOC), kiintoainetta ja ravinteita. Tästä huolimatta kemiallisen käsittelyn optimointia ei ole tehty hajakuormitukselle, kuten turvetuotannon valumavesille, minkä seurauksena valumavesien puhdistustuloksissa on suurta vaihtelua. Tässä väitöstyössä tutkittiin markkinoilla saatavilla olevien kemikaalien sopivuutta turvetuotannon humuspitoisille valumavesille. Tutkimuksessa testattiin epäorgaanisia (ferrisulfaatti, alumiinisulfaatti ja näiden sekoitus) ja orgaanisia (polyDADMAC, polyamiini, kitosaani ja tanniinipohjaisia polymeerejä) koagulanttikemikaaleja. Tutkimuksessa selvitettiin koagulanttien annostarpeet sekä erilaisten prosessiparametrien (vedenlaatu, sekoittaminen, pH ja lämpötila) vaikutus koagulanttien toimintaan. Laboratoriotutkimusten lisäksi väitöstyö sisälsi kenttämittauksia turvetuotannon valumavesien tyypillisten kemiallisen vesienkäsittelyn prosessiparametrien selvittämiseksi. Tutkituista koagulanteista rautasulfaatti oli tehokkain. Se tuotti hyvin laskeutuvaa flokkia ja poisti parhaiten valumavesien orgaanista ainesta. Rautasulfaatti vaati kuitenkin selkeästi suuremman annostuksen kuin esimerkiksi polyDADMAC ja kitosaani. Lisäksi puhdistettuun veteen jäi paljon rautaa ja vesi oli hapanta. Orgaanisilla kemikaaleilla saavutettiin myös kohtalainen/melko hyvä puhdistustulos, mutta lisää tutkimusta tarvitaan ennen kuin ne voivat olla vaihtoehtona epäorgaanisille kemikaaleille. Turvetuotannon valumaveden laatu vaihteli paljon. Valumaveden orgaanisen aineen määrän vaihtelulla oli suurin vaikutus kemikaalin annostukseen ja puhdistustulokseen. Sekoituksista kemiallisen käsittelyn flokkulaatiovaiheen sekoituksella oli suurempi vaikutus puhdistustulokseen kuin koagulaatiovaiheen sekoituksella. Tutkituilla turvetuotantoalueilla ei kuitenkaan ollut tällä hetkellä riittävää sekoitusta flokkulaatiovaiheessa. Tässä väitöstyössä esitetään parannuksia kemiallisen käsittelyn optimointiin paremman ja vakaamman puhdistustuloksen aikaansaamiseksi humuspitoisille vesille.

Doctor of Philosophy / Department of Horticulture, Forestry, and Recreation Resources / Kimberly A. Williams / The use of calcined clays contributes properties of nutrient and water retention to soilless root media, which varies greatly depending on the parent clay and calcining treatment. This research characterized phosphate (PO[subscript]4) sorption of various calcined clay products, including low volatile and regular volatile material (LVM and RVM) 2:1 Attasorb clays (Engelhard Corp.), 2:1 Terra Green LVM clays (Oil-Dri Co.), and Turface (Profile Products LLC) at various particle sizes; 1:1 kaolin clays (Thiele Kaolin Co.) in powder form, and diatomaceous earth (Diatomite, Eagle Picher Minerals, Inc.). Three of the calcined materials, Terra Green montmorillonite and Attasorb attapulgite (which had high PO[subscript]4-sorption based on isotherms), and diatomaceous earth (which had negligible PO[subscript]4-sorption) were evaluated as components of soilless root media in two separate greenhouse experiments. The effect of the calcined materials, rate of incorporation (0%, 5%, 10% and 20% by volume in a mix with peat and perlite), and PO[subscript]4-P application rate (0, 5, 15, 45 mg.L[superscript]-1 PO[subscript]4-P) on plant growth, effluent P content and water use were determined during production and post-production of Impatiens wallerana Hook f. 'Tempo Rose'. The calcined materials varied in their ability to adsorb PO[subscript]4-P and generally yielded L-type isotherms. Laboratory results indicated potential for substantive P retention by several of the calcined materials when used in container production. For most materials, PO[subscript]4-P sorption did not show pronounced pH dependence. During production and post-production, the test materials not only improved PO[subscript]4-P retention but also water retention and water use efficiency while still maintaining optimal physical properties at incorporation rates of 5 to 10%. Diatomaceous earth resulted in PO[subscript]4-P retention not significantly different from the calcined clays.

Reducing the rates of greenhouse gas (GHG) emissions is critical in combatting global climate change. Carbon dioxide (CO2) and methane (CH4) are the two most important carbon-based GHGs, for their atmospheric warming potential. Wetlands such as the Florida Everglades play major roles in the global carbon cycle, as varying hydrologic conditions lead to differential production rates of these two GHGs. This study measured CO2 and CH4 emissions in a re-created Everglades ridge-and-slough wetland, where water levels were controlled to reflect natural flood patterns. As expected, lower elevations were flooded longer and produced more CH4, while higher elevations produced more CO2. Since CH4 has a relatively high global warming potential, CO2 production would need to be 70 times that of CH4, to balance their GHG output. The average ratio of CO2 to CH4 across elevations was 22.0 (mol:mol), indicating that future water management within wetlands should consider GHG production potential.

The area at and around the Falun copper mine has always been of great interest. To begin with it was the valuable ore that drew people to the area. Now it is the historical, archaeological and environmental aspects that draw researchers from different fields of study to Falun. Peat cores were taken in several peatlands throughout an area extending toward about 2 kilometres to the west, southwest and south of the Falun mine. One core was selected for more extensive studies including plant macrofossil analysis, loss on ignition (LOI) and 14C – analysis. These methods are combined to give a picture of the environmental conditions at different periods in time, using plants and their preferred growth environment as an aid. The untouched environment changing into the well-known mining landscape that prevailed in the hey-day of the mine, with the change being the focal point, is the reason for this study.The cores presented in this thesis generally show lake areas drying up and transforming into peatlands, some peatlands may however have been formed in other ways. The location chosen for further studies is now almost transformed to a forest floor. This study provides a solid foundation for further studies as well as adds more information to existing knowledge. However, more research is needed to fully understand how the environment changed due to the opening of the mine. / Området vid och runt Falu koppargruva har alltid varit av stort intresse. Till en början var det den dyrbara malmen som lockade människor till platsen. Numer är det de historiska, arkeologiska och miljörelaterade aspekterna som lockar forskare från olika forskningsfält hit. Torvkärnor togs från flera torvmarker inom ett område som sträcker sig ungefär 2 kilometer i väst-, sydväst-, och sydlig riktning från Falu gruva. En torvkärna valdes ut för mer omfattande undersökningar, dessa inkluderar växt-makrofossil-analys, LOI och 14C – analys. Dessa metoder kombineras för att få en bild av de rådande miljöförhållandena vid olika tidpunkter, genom att använda växters föredragna växtplats som hjälp. Det är hur den orörda naturen förändrats till det välkända gruvlandskapet som rådde under gruvans storhetstid, med förändringen i centrum, som är anledningen till denna studie.Torvkärnorna som visas i denna rapport visar i stort sett hur sjömiljöer torkat ut och förändrats till våtmarker, vissa våtmarker kan dock ha utvecklats på annat sätt. Den plats som valdes ut för vidare studier har idag nästan helt omvandlats till skogsmark. Denna studie ger en stadig grund för vidare studier och tillför viss information till den redan befintliga. Det behövs dock mer forskning för att fullt ut förstå de miljöförändringar som gruvdriften medförde.

Cyclamens are deemed an essential cold season crop for supplementing the income of commercial growers during winter. However, cyclamens have the reputation of being a demanding commercial crop mainly due to difficulty in successful crop cultivation, lengthy production time and production costs. The economic and environmental landscape in South Africa dictates that careful consideration be given to reducing production time and costs, but still improving the quality of the commercial crop for market readiness. Growth medium are considered an important factor contributing significantly to the quality of commercially grown container cyclamens in a controlled environment. The focus of this study was on establishing the most suitable growth medium for commercially grown cyclamens in a South African environment in order to improve the quality of the commercial crop. Only one F1 variety of cyclamen was used as the sample population with a sample size of five plants per growth medium mixture planted according to a randomised block design in a specified area within a greenhouse. Seven commercially available growth medium mixtures, five locally available and two imported, were subjected to a typical production cycle of commercial cyclamens in a controlled greenhouse. The growth medium mixtures for comparison were Cyclamen Mix; 45 Mix; 50% Cyclamen Mix - 50% 45 Mix; 49 Mix; 7 Mix; coarse coir; Klasmann base 4 Substrate mix . The measuring instrument used in the study was adapted from existing instruments used in the comparison of cyclamens and growth medium. It included various measurements and observations: Plant height, plant diameter, plant weight, number of leaves, leaf width, foliage fresh weight, number of flowers, diameter of tuber and root fresh weight. The results obtained in the comparison determine the most suitable growth medium for container cyclamens for South African circumstances. The physical properties of peat retain water for a longer time which is beneficial for the production of container cyclamen. The results of this study therefore indicate that growth mediums containing peat performed better than mediums containing no peat. / Agriculture and  Animal Health / M.Sc. (Ornamental Horticulture)

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