The Gulf Coast of Texas has been proposed as a high capacity storage region for geologic sequestration of anthropogenic CO₂. The Miocene section within the Texas State Waters is an attractive offshore alternative to onshore sequestration. However, the stratigraphic targets of interest highlight a need to utilize fault-bounded structural traps. Regional capacity estimates in this area have previously focused on simple volumetric estimations or more sophisticated fill-to-spill scenarios with faults acting as no-flow boundaries. Capacity estimations that ignore the static and dynamic sealing capacities of faults may therefore be inaccurate. A comprehensive fault seal analysis workflow for CO₂-brine membrane fault seal potential has been developed for geologic site selection in the Miocene section of the Texas State Waters. To reduce uncertainty of fault performance, a fault seal calibration has been performed on 6 Miocene natural gas traps in the Texas State Waters in order to constrain the capillary entry pressures of the modeled fault gouge. Results indicate that modeled membrane fault seal capacity for the Lower Miocene section agrees with published global fault seal databases. Faults can therefore serve as effective seals, as suggested by natural hydrocarbon accumulations. However, fault seal capacity is generally an order of magnitude lower than top seal capacity in the same stratigraphic setting, with implications for storage projects. For a specific non-hydrocarbon producing site studied for sequestration (San Luis Pass salt dome setting) with moderately dipping (16°) traps (i.e. high potential column height), membrane fault seal modeling is shown to decrease fault-bound trap area, and therefore storage capacity volume, compared with fill-to-spill modeling. However, using the developed fault seal workflow at other potential storage sites will predict the degree to which storage capacity may approach fill-to-spill capacity, depending primarily on the geology of the fault (shale gouge ratio – SGR) and the structural relief of the trap. / text

Lower Paleozoic strata in southeastern Kansas, southwestern Missouri and northern Oklahoma are predominantly marine carbonates that comprise portions of three regional flow systems. Groundwaters in these three adjacent systems exhibit extreme chemical and isotopic variations that delineate large-scale fluid mixing processes and two distinct mechanisms for the generation of saline fluids. Hydrodynamic and geochemical data closely correlate with geographic location and indicate that each system contains waters of markedly different origins. Results of elemental and isotopic mass balance modeling demonstrate that fluid mixing processes exert a fundamental control on groundwater compositions over the 40,000 km² study area. This quantification of groundwater mixing provides an important basis for determining endmember water compositions and evaluating hydrologic models for these flow systems. The three endmember groundwaters are as follows. 1) Dilute modern-day meteoric waters of the Ozark Plateaus aquifer system, recharged to southern Missouri. The evolution of this groundwater is dominated by interaction with host limestone and dolomite aquifer rocks. 2) Eastward migrating, saline Na-Ca-Cl groundwaters from the northern part of the Western Interior Plains aquifer system in central Kansas. These groundwaters are of meteoric origin with distant recharge areas. Salinity is acquired via the subsurface dissolution of Permian halite and subsequent water-rock interaction with silicate minerals. The chemical signature of these groundwaters, coupled with the presence of brines resulting from the dissolution of Permian halite in central Kansas, allow development of a model for the formation of saline Na-Ca-Cl fluids, a common component of many sedimentary basins. Additionally, the large-scale topographically driven flow of the northern part of this aquifer system is a modem analog for models of similar ancient systems. 3) Na-Ca-Cl brines in north-central Oklahoma. In contrast to the other saline endmember, the geochemical signature of endmember 3 groundwater, integrated with hydrogeologic data, indicate that this groundwater may represent a marine-derived brine from the deep Anadarko Basin. / text

Aluminized steel pipes are expected to have a long service life, e.g. 75 years. Spiral ribbed aluminized pipes (SRAP) have been widely specified and used by the Florida Department of Transportation (FDOT) for drainage of runoff water. Confidence in the long term durability of SRAP has been challenged by recent unexpected early corrosion failures in various Florida locations. SRAP premature corrosion incidents have occurred in two modalities. Mode A has taken place in near-neutral soil environments and has often been associated with either gross manufacturing defects (i.e. helical cuts) or corrosion concentration at or near the ribs. Mode B took place in pipes in contact with limestone backfill and corrosion damage was in the form of perforations, not preferentially located at the ribs, and not necessarily associated with other deficiencies. These failures motivated this research. The objectives of this work are to establish to what extent the Mode A corrosion incidents can be ascribed to manufacturing defects, that can be rectified by appropriate quality control, as opposed to an intrinsic vulnerability to corrosion of regularly produced SRAP due to ordinary forming strains and to determine the mechanism responsible for Mode B corrosion including the role that limestone backfill played in that deterioration. To achieve those objectives, laboratory experiments were conducted to replicate the conditions for Mode A and Mode B. Overall, the findings of this and previous work suggest that much of the corrosion damage observed in the Mode A incidents were promoted more by manufacturing deficiencies and less by any possible inherent susceptibility of corrosion at the ribs of SRAP that was produced following appropriate quality control. Experiments to explore the causes of Mode B corrosion showed that high pH values, sufficient to cause dissolution of the passive film on aluminum, can develop under exposure of limestone to flowing natural water. The findings substantiate, for the first time, an important vulnerability of aluminized steel in limestone soils and provide an explanation for the rapid onset deterioration observed at the field under Mode B. The findings also provide strong evidence in support of service guidelines to disallow the use of limestone bedding for aluminized steel pipe, including SRAP.

Co-produced water from the oil and gas industry represents a significant waste stream in the United States. Produced water is characterized by high levels of total dissolved solids (TDS), dissolved organics and oil and grease. Among the wide variety of organics present in the water, the concentration of hazardous substances such as benzene, toluene, ethylbenzene, and xylenes (BTEX) can reach 600 mg/L and the concentration of non-hazardous carboxylate can be as high as 10,000 mg/L (API, 2002). Regulations governing the disposal of produced water are tightening and the interest in reusing treated produced water is increasing in the United States particularly in regions with scarce water supplies. In order to reuse produced water, removal of both the inorganic dissolved solids and hazardous organics such as BTEX may be necessary. The main goal of this research was to investigate the feasibility of using a combined physicochemical/biological treatment system to remove the organic constituents present in saline produced water. In order to meet this objective, two separate biological treatment techniques were investigated: a vapor phase biofilter (VPB) to treat the regeneration off-gas from an upstream surfactant-modified zeolite (SMZ) adsorption system and a membrane bioreactor (MBR) to treat the carboxylate and BTEX constituents that penetrate an upstream SMZ system. Each of the biological pretreatment systems was investigated first in the laboratory treating synthetic produced water and then in the field coupled to an SMZ adsorption system treating produced water. Both of the biological treatment systems were capable of removing the BTEX constituents both in the laboratory and in the field over a range of operating conditions. For the VPB, separation of the BTEX constituents from the saline aqueous phase yielded high removal efficiencies. However, carboxylates remained in the aqueous phase and were not removed in the combined VPB/SMZ system. In contrast, the MBR was capable of directly treating the saline produced water and simultaneously removing the BTEX and carboxylate constituents. The major challenge of the MBR system was controlling membrane fouling, particularly when the system was treating produced water under field conditions.

It is recognised by society that freshwater resources play a major role in economic development and in maintaining life supporting ecosystems services. Transboundary river basins cover about 45% of the earth’s land surface and their governance is therefore of critical importance. Transboundary freshwater resources are considered a common-pool resource. Collective action is therefore needed in order to supply both public and private goods from these resources but is yet in short supply. This thesis intends to analyse a complementary framework to the common Integrated Water Resources Management (IWRM) approach with the objective of enhancing investments in collective action to address this dilemma. Results indicate that transboundary water resources management in itself can be identified as a regional public good. The results also indicate that IWRM has been promoted as a standard management concept; often without first having identified and agreed the objectives of the intended multiple uses of water. Outcomes related to IWRM at the transboundary scale are therefore difficult to identify and evidence points towards continued water quality degradation at a global scale and development opportunities not achieved. Two different tools for how to assess the generation of benefits from cooperation are presented in this thesis including an institutional assessment framework adapted to transboundary institutions. Together these steps make up an outcome-driven approach that clarifies the value of water in all management and development stages. Through such an outcome-driven approach, water issues can provide the incentives necessary in order to identify cooperative paths and thus become important factors in negotiations to establish effective regional governance regimes. This would take the broader political, economic and geographical context into consideration thus supporting a process towards more integration of interests between countries.

Escherichia coli is a bacterial species that lives in the gut of all warm-blooded animals, fish, birds as well as reptiles and is commonly used as an indicator of fecal contamination in water. This project assessed currently used culture based media for the detection of E. coli in irrigation waters used in Arizona and California, and will present recommendations towards the most reliable media for the evaluation of irrigation waters used for produce. Currently, no microbial indicator standards exist for irrigation waters used for produce production in the United States. The produce industry suggests that the recreational water standard guideline (126 E. coli/100 ml) established by the United States Environmental Protection Agency (USEPA) be used. There is concern that the false positive rate of E. coli detection may be high in these waters giving false indications of the level of risk from enteric pathogens. This project evaluated three commercially available media for E. coli detection to test irrigation waters from three agricultural areas (Yuma and Maricopa, AZ and Imperial Valley, CA) and then assessed false positive rates by utilizing Polymerase Chain Reaction (PCR) and DNA sequencing of the bacterial isolates. The media that were chosen for evaluation were (1) MI Agar, (2) IDEXX Colilert Quanti-Tray® and (3) m-ColiBlue24® broth, all evaluation media accepted by the USEPA and widely used in the monitoring of irrigation water quality by the produce industry. Four hundred and fifty 1-L irrigation water grab samples were collected between March 2012 and November 2012. The samples were analyzed for both cultural counts and water quality parameters including temperature, salinity and pH. Isolates positive and negative for E. coli were then selected and assessed utilizing PCR and DNA sequencing. The false positive rate of each method was found to be high, with MI Agar, m-ColiBlue24® broth and the IDEXX Colilert Quanti-Tray® at an accuracy of 67%, 72%, and 51% respectively. A false positive result is reported when presumptive E. coli sub cultured from the media is found to be non-E. coli through molecular analysis. Overall the IDEXX Colilert Quanti-Tray® performed at a greater rate of accuracy than the other two media evaluated, however, high false positive rates may lead to inaccurate assessment of water quality.

This dissertation approaches the geopolitics of river infrastructure in the Indus Basin through the structured interaction of "hydraulic regionalism" and "technocratic developmentalism". The former occurs when regional elites feel their access to river resources are threatened by upstream infrastructure development. The latter occurs when technocratic elites underplay the geopolitics of regional vulnerability by stressing the overall integrated development of river resources to maximize utility. The dissertation interprets archival, legal, and ethnographic data regarding the negotiation and adjudication of the Indus Waters Treaty between India, Pakistan, and the World Bank, as well as the implementation of the Indus Basin Development Fund Agreement. The dissertation also analyzes upstream/downstream tension between the Pakistani provinces of Punjab and Sindh. The contributions of this dissertation are in the fields of post-colonial state theory, the political ecology/economy of environmental knowledge, the geopolitics of river disputes, and Marxist methodology.

Diese Arbeit behandelt die Charakterisierung der Habitate und die Langzeit-Entwicklung über sechs Jahrzehnte der Makrophytenvegetation nordwestdeutscher Bäche und Flüsse, um zum Wissen über die Ökologie aquatischer Makrophyten beizutragen und sie als Bioindikatoren zu nutzen. Siebzig Bäche und Flüsse der Regionen Ems-Hunte Geest, Lüneburger Heide, Allerflachland, nördliches Harzvorland, Fuß des Weser-Leine Berglandes und ostholsteinisches Hügelland sind Bestandteil der Studie, wobei der Schwerpunkt auf der überregionalen Betrachtungsebene liegt. Aus der Analyse der Zusammensetzung und Verbreitung der Makrophytengesellschaften im Zusammenhang mit Gewässergröße und physikalischen und chemischen Wasser- und Sedimenteigenschaften schlossen wir, dass Gewässertiefe und Fließgeschwindigkeit von den gemessenen Variablen den größten Einfluss auf die heutige Gesellschaftszusammensetzung haben, gefolgt vom Gehalt pflanzenverfügbaren Phosphors im Sediment. Es ist jedoch nicht auszuschließen, dass vor der im Untersuchungsgebiet seit den 1950ern stattfindenden, starken Intensivierung der landwirtschaftlichen Nutzung, als noch ausgeprägtere Gradienten bei den Nährstoffgehalten der Fließgewässer existiert haben, chemische Größen einen stärkeren Einfluss auf die Makrophytenvorkommen hatten als heute. Mittels semi-permanenter Dauerflächen haben wir den Vegetationswandel zwischen den 1950ern und 2010 untersucht und einen dramatischen Rückgang der Artenvielfalt festgestellt (der Gesamtartenpool sank um 27.5 % von 51 auf 37 Hydrophytenarten, die Artenzahl pro Aufnahmefläche um 19.4 % von 4.7 auf 3.8 Arten), begleitet von einem umfassenden Bestandsumbau vom Vorherrschen wurzelnder (v.a. potamider) Arten zur Dominanz freischwimmender (v.a. lemnider) Arten. Oligotraphente Arten wie Potamogeton gramineus und P. polygonifolius sind in den Probeflächen ausgestorben und die mesotraphenten Arten Myriophyllum alterniflorum und Ranunculus peltatus in ihrer Auftretenshäufigkeit um mehr als 50 % zurückgegangen, während die eutraphenten Arten Myriophyllum spicatum und Spirodela polyrhiza um mehr als 100 % zugenommen haben. In den Artmerkmalen Blattausdauer und spezifische Blattfläche (SLA) wurden Änderungen festgestellt: In den historischen Makrophytenbeständen der 1950er waren immergrüne Arten und Arten mit dünnen Blättern oder solchen mit viel arenchymatischem Gewebe häufig (große SLA), während die rezenten Bestände von 2010 durch sommergrüne Arten und solche mit robuster Struktur (geringe SLA) gekennzeichnet sind. Die Veränderungen in der Arten-zusammensetzung waren am tiefgreifendsten in der Region Ems-Hunte Geest, wo weitläufige Niedermoore durch Entwässerung insbesondere seit der Eindeichung des Dümmer Sees (1953) intensiv bewirtschaftetem Agrarland gewichen sind, und weniger ausgeprägt in der Lüneburger Heide, einer der wenigen Tieflandsregionen Deutschlands, in der noch Fließgewässer mit kaum durch den Menschen veränderter Struktur zu finden sind. Auf der syntaxonomischen Ebene zeigte die Anwendung zweier unterschiedlicher pflanzensoziologischer Klassifikationssysteme tiefe Veränderungen in der Struktur der Makrophytengesellschaften über sechs Jahrzehnte auf. Alle dokumentierten Vegetations-bestände konnten einer der Klassen Potamogetonetea, Lemnetea, Phragmitetea oder Fontinalietea zugeordnet werden. Während Batrachietalia/Batrachion und Potamogetonetalia /Potamogetonion-Bestände stark zurückgegangen sind, haben Nymphaeetalia/Nymphaeion-Gesellschaften zugenommen. Die beobachtete Zunahme pflanzensoziologisch schwach charakterisierter Bestände (Fragmentgesellschaften) deutet auf Verluste bei den hoch-spezialisierten Arten hin. Im Schnitt waren sich die rezenten Vegetationsbestände signifikant ähnlicher (SBC=0.25) als die historischen (0.22), was eine Homogenisierung der Fließgewässervegetation Nordwestdeutschlands offenbart. Beschleunigte Eutrophierungsprozesse in den Gewässern und wasserbauliche Maßnahmen in der intensiv genutzten Kulturlandschaft haben zu einer Uniformierung der Fließgewässerhabitate geführt, worin neben häufigen Störereignissen die Hauptursache für die Verluste in Artenreichtum und Vielfalt der Makrophytenvegetation gesehen werden kann. Weitere Anstrengungen zur Reduzierung der Nährstofffrachten, sowie eine Erhöhung der Habitatheterogenität durch strukturverbessernde Renaturierungsmaßnahmen und ökologisch verträgliche Unterhaltungstechniken und -zeitpunkte sind notwendig, um den Diversitäts-rückgang in der Makrophytenvegetation nordwestdeutscher Bäche und Flüsse aufzuhalten und umzukehren. Eine artenreiche Vegetation ist ein wichtiger Baustein in Fließgewässer-Ökosystemen, deren Funktionsfähigkeit nicht zuletzt auch für das menschliche Wohlergehen von Bedeutung ist.

The Devils Lake defection of 2005 demands a re-evaluation of the venerable Boundary Waters Treaty (BWT) between Canada and the United States. Why was the long-successful water agreement unable to solve this relatively minor dispute? More importantly, given irregularities between theoretical assertions and institutional history, what theory of international relations best explains a cooperative agreement that spans a near-century? Due to the complexities of shared river systems, any theory that seeks to explain international cooperation must adequately encompass three separate sources of state motivation. First, it must explain the technical, basin-position-driven realities that affect state attitudes towards negotiations. Second, it must explain the longer-term strategic factors that can inspire states to accept immediate losses for subsequent gains. Finally, it must acknowledge domestic sources of influence and understand how these forces constrain the state vis-à-vis others. This paper argues that liberalism, as defined by Andrew Moravcsik, is the best theoretical candidate. This is proven by comparing interpretations of the BWT history through realist, neoliberal, constructivist, and liberal lenses. After identifying and examining each theory's strengths and weaknesses, liberalism emerges as the most holistic view and should be favoured as a primary explanatory theory. Liberalism's theoretical underpinnings – interest group politics – best handles the technical, strategic, and domestic influences that affect Canada-US water relations. Whether examining what prompted efforts to initiate a water-sharing agreement, explaining the agreement's final structure, determining the impetus for continued cooperation, or identifying the incentives to finally break from treaty obligations, liberalism provides the most satisfying solutions. Though derived from the Canada-US border relationship, liberalism's superiority is not limited to the North American watershed. Because the factors examined are common to all shared international river systems and the paper's results are scalable, this suggests that liberalism will continue to be the appropriate primary IR theory to employ when examining state decision-making regarding water-sharing agreements.

The Late Jurassic Brae oilfields in the South Viking Graben of the northern North Sea contain naturally high concentrations of carbon dioxide (up to 35 mol %). Fields immediately adjacent to the graben bounding fault display the highest concentrations, with CO2 content decreasing eastward into the basin. It is thought the CO2 was introduced into the region via this fault. This thesis examines the possible source of the high CO2 present in the region, focusing on the graben margin fault as a potential conduit for CO2 flux from depth Investigation of cored sections penetrating the graben bounding fault revealed numerous carbonate cemented fracture arrays. The morphology of the fractures and cements is attributed to hydraulic fracturing induced by episodic release of overpressured fluids up the margin fault from depth. Periods of rapid subsidence omnipresent throughout the tectonic history of the graben are conducive to the generation of overpressure; a feature commonly reported in the region. Samples from the carbonate fracture cements were analysed using a host of techniques, including SEM, EMPA, fluid inclusion, and stable δ13C ‐ δ18O analyses. Using SEM analysis, at least five generations of dolomite cement with concomitant iron sulphide were observed. Cement chemistry and textures indicate precipitation from concentrated CO2–rich fluids. A reported high salinity basinal influx from depth concomitant with proposed CO2 charge into the region ~70 Ma is a probable source for the dissolved solids subsequently precipitated as carbonate in the fracture networks. Fluid inclusion analysis provided sufficient evidence to suggest the influx of hot fluids into the region, presumably sourced from deep in the margin fill. Two distinct δ13C vs. δ18O trends are observed in the isotope data from four wells studied. The trends are interpreted as differential mixing between ascending basinal fluids rich in dissolved inorganic carbon and in situ formation waters dominated by organically derived carbon following the onset of thermal decarboxylation in the Kimmeridge Clay Formation. Dissolution of Zechstein carbonates underlying the region is a credible source for the isotopically heavy CO2 found adjacent to the graben margin (δ13CCO2 = ‐2 to ‐5 ‰) and incorporated into the carbonate cements. Inferred variations in fluid mixing from well to well have implications on the variability of fluid flow along the graben margin with respect to contrasting fault morphologies. A Rayleigh fractionation model accommodating CO2 degassing from a hot ascending isotopically heavy fluid can be invoked to explain the observed carbon‐oxygen isotopic covariations in the fracture cements. Geochemical modelling simulating the ascent of CO2‐rich waters suggests degassing has limited impact on precipitation volumes, with fluid‐rock reactions the most likely driver for extensive carbonate mineralisation observed.