Eight agricultural catchments in south Sweden were investigated for factors that may affect phosphorus (P) load and retention in the downstream situated wetlands (WL). P load is known to affect retention, and is determined by hydrological and geographical catchment characteristics. The wetlands were small (0.02-0.88%) in relation to their catchments (CA) and varied in design. Net sedimentation and P retention was determined with sedimentation plates during one year. The variables that best explained differences in particles and TP retention were the hydraulic load (q), TP load and the wetland length to width ratio. Contrary to expectations there was no correlation between factors that could be associated with erosion (i.e. slope and soil clay content) and retention of neither particles nor TP. Generally, the highest amounts of settled particles and P were found close to the wetland inlets, but soil disturbance (i.e. tillage) and high q increased the settling distance. It was likely that the smallest clay particles were too unaggregated to settle within these wetlands. Factors not included, such as wetland vegetation and bioturbation may have a large impact on P retention and this should be further investigated. The study also points to the difficulties in scaling down geological and P loss data from a regional to a local scale, as there can be large local deviations from the regional standard values. An easy method for identification of local “hotspots” for P losses should be of value for planning the location of future wetlands.

Mercury (Hg) which originates from global emissions to the atmosphere can deposit far away from the source. There is often a weak correlation between Hg deposition and concentrations in runoff, therefore catchment specific parameters might be of importance in controlling the amount of Hg ending up in watercourses and fish. Total mercury (THg) and methylmercury (MeHg) concentrations in watercourses are correlated to organic matter (OM), and in this study total organic carbon (TOC) is used as a proxy for OM. This study covers data from 125 watercourses in Sweden, and investigates the impact of e.g. Topographic Wetness Index (TWI), forest type, soil and bedrock types, deforestation and catchment size on the THg and MeHg concentrations as well as on the residuals from the regression between THg and TOC. Previous studies have found strong correlations between THg and OM as well as MeHg and OM but few previous studies have studied influences of catchment specific factors on THg and MeHg runoff concentrations with data of this large spatial and temporal scale. The catchment characteristics were extracted through ArcMap and projection to latent structures (PLS) models were created to evaluate what characteristics had the strongest influence on the variation in THg and MeHg concentrations as well as on the THg/TOC residuals. A strong correlation was found between THg and TOC, but a weaker one between MeHg and TOC. The MeHg concentrations were found to be dependent on variables which co-vary with TOC, as well as on latitude. The negative impact of latitude on MeHg concentrations could be due to methylation being temperature dependent or reflecting a spatial variation in Hg deposition from north to south of Sweden. Amount of deforestation was found to have an impact on the THg concentrations, indicating that deforestation leads to larger THg fluxes from soil to stream. The fact that variables measuring OM content in the streams were strongly influencing THg and MeHg concentrations, and the fact that few catchment characteristics were of importance, indicate the high importance of OM in explaining THg and MeHg also at this large spatial and temporal scale. / Studien sammanfattar hur halter av kvicksilver, och dess relation till organiskt material, i vattendrag påverkas av olika landskapsvariabler. Få tidigare studier har studerat hur kvicksilverhalten i vattendrag varierar beroende på avrinningsområdets karaktär i så stor skala, vad gäller antal områden och antal mätvärden, som i denna studie. Kvicksilver (Hg) är ett skadligt ämne för människor och natur, eftersom det i sin biotillgängliga form, metylkvicksilver (MeHg), är ett nervgift som kan orsaka stor skada på centrala nervsystemet. I de flesta vattendrag i Sverige är den uppmätta kvicksilverhalten i fisk högre än världshälsoorganisationens rekommenderade gränsvärden för fisk som föda. Kvicksilver härstammar från globala utsläpp till atmosfären som kan falla ned långt ifrån utsläppskällan. Då det ofta inte finns något rakt samband mellan kvicksilvernedfallet och de koncentrationer som återfinns i avrinnande vatten så kan områdesfaktorer och aktiviteter i de lokala avrinningsområdena ha stor betydelse för hur mycket kvicksilver som hamnar i våra ytvatten och sedan i fisken. Ett starkt samband har påvisats mellan mängden organiskt material i vattendrag och koncentrationen av totalkvicksilver (THg). I denna studie testas om sambandet mellan kvicksilver och organiskt material, mätt som total organiskt kol (TOC), kvarstår över lång tid (upp till 17 år) och hög rumslig upplösning (125 avrinningsområden). Eftersom ett relativt starkt samband återfanns fokuserade den här studien på att vidare utreda hur sambandet mellan THg och TOC, samt koncentrationer av MeHg, påverkas av områdesfaktorer i de olika avrinningsområdena. Det undersöktes hur skogstyp, jordarts- och bergartstyper, skogsavverkning, avrinningsområdets storlek samt Topographic Wetness Index (TWI, ett mått på hur topografi och markfuktighet är fördelat inom ett avrinningsområde), påverkar koncentrationer av total- och metylkvicksilver samt relationen mellan totalkvicksilver och organiskt material. Information om avrinningsområdena togs fram i GIS och statistiska modeller för hur områdesfaktorer påverkar kvicksilverkoncentrationer skapades genom PLS analyser (Projection to Latent Structures). Latitud visade sig ha en negativ påverkan på MeHg koncentrationerna; desto högre latitud desto mindre MeHg, vilket kan bero på att metylering är temperaturdriven process och/eller att reflektera en variation i Hg deposition från norra till södra Sverige. Studien kan sammanfattningsvis säga att inget samband hittades mellan de övriga landskaps-variablerna som undersökts i studien och kvicksilver koncentrationer.

The seasonal variation and landscape regulation of dissolved organic carbon (DOC) concentrations in streams have been studied in two watersheds in the boreal zone. The seasonal variation was found to be highly correlated to variations in runoff. An increase in runoff was always accompanied with an increase in DOC concentration. However, there were indications that the TOC concentration was restricted by the soil TOC pool during snowmelt. The main factors affecting DOC exports varied between seasons. During winter baseflow the spatial variation in DOC exports was strongly influenced by wetland coverage, during snowmelt the exports were correlated to factors describing the size and location of the catchment, and during the snow-free season they were heavily affected by the proportions of wetlands and forests in the catchments. Small headwaters had the highest terrestrial DOC export, per unit area. The properties of the DOC changed during spring flood, towards lower molecular weight and more aliphatic compounds. These changes affected the bioavailability of the DOC, which increased during spring flood. There were also differences in the DOC properties between wetlands and forest soils; the forested soils yielded DOC with lower molecular weight (measured as 254 nm/365 nm light absorbance ratios), largely from superficial layers that were activated during high flow events, while wetland soils generally provided a more constant carbon source with higher molecular weight. The majority of the DOC was exported by wetlands, but most of the short-term bioavailable DOC (BP7) was derived from the forests, during the spring flood period, indicating that bacterial production in streams and lakes is likely to be almost entirely based on DOC exported from forested areas during, and some time after, the spring flood event.

Human related activities have influenced the rivers of the southern Western Cape since as early as the 1700’s. As there is no detailed information available on ecological status of the Holsloot River, a tributary of the Breede River, this study aimed to gain insight into the effect of impacts associated with human activities on the habitat integrity of this river. The study intended to understand how seasonal changes, catchment characteristics and events are reflected in the ecological status of habitats along the river by applying bio-monitoring and river health measurements at selected sites in the upper, middle and lower reaches of the Holsloot River and compare the results to that of an undisturbed reference site. Results obtained in this study are compared with data gathered in 2008/2009 to determine if the ecological status of the river had changed in the period between the two sampling times. The study included assessment of the ecological status of the river based on standard bio-monitoring protocol (SASS5, IHI, IHAS and VEGRAI) as well as in situ water quality analysis (pH, dissolved oxygen, electrical conductivity and total dissolved solids). The construction of the instream Stettynskloof Dam changed the configuration of the riparian zone and river channel in the upper catchment area. Agricultural- and other human related activities, with consequent water abstraction, non-point-source pollution, loss of riparian vegetation, as well as dense stands of alien invader plants influence flow patterns and affects river ecology, especially in the dry summer months. Providing sufficient stream flow and adequate water levels, human related activities can create a larger variety of habitat types available that can support larger biodiversity and higher productivity. The level of inundation and stream flow, influenced by water abstraction as well as irrigation return-flow from extensive drainage systems especially in the dry months, contribute to the loss of biodiversity in the middle and lower reaches of the river. Where the upper reaches of the river are largely natural with few modifications, the habitat integrity deteriorates in the middle reaches so much so that ecosystem functioning are collectively impaired in lower reaches due to human related impacts. Sensitive macro-invertebrates found at lower seriously impacted parts of the river however, were in all probability washed down from lower impacted upstream habitats and may expectedly be able to again occupy habitats downstream if water quality and habitat availability improves. / Environmental Sciences / M. Sc. (Environmental Science)

Human related activities have influenced the rivers of the southern Western Cape since as early as the 1700’s. As there is no detailed information available on ecological status of the Holsloot River, a tributary of the Breede River, this study aimed to gain insight into the effect of impacts associated with human activities on the habitat integrity of this river. The study intended to understand how seasonal changes, catchment characteristics and events are reflected in the ecological status of habitats along the river by applying bio-monitoring and river health measurements at selected sites in the upper, middle and lower reaches of the Holsloot River and compare the results to that of an undisturbed reference site. Results obtained in this study are compared with data gathered in 2008/2009 to determine if the ecological status of the river had changed in the period between the two sampling times. The study included assessment of the ecological status of the river based on standard bio-monitoring protocol (SASS5, IHI, IHAS and VEGRAI) as well as in situ water quality analysis (pH, dissolved oxygen, electrical conductivity and total dissolved solids). The construction of the instream Stettynskloof Dam changed the configuration of the riparian zone and river channel in the upper catchment area. Agricultural- and other human related activities, with consequent water abstraction, non-point-source pollution, loss of riparian vegetation, as well as dense stands of alien invader plants influence flow patterns and affects river ecology, especially in the dry summer months. Providing sufficient stream flow and adequate water levels, human related activities can create a larger variety of habitat types available that can support larger biodiversity and higher productivity. The level of inundation and stream flow, influenced by water abstraction as well as irrigation return-flow from extensive drainage systems especially in the dry months, contribute to the loss of biodiversity in the middle and lower reaches of the river. Where the upper reaches of the river are largely natural with few modifications, the habitat integrity deteriorates in the middle reaches so much so that ecosystem functioning are collectively impaired in lower reaches due to human related impacts. Sensitive macro-invertebrates found at lower seriously impacted parts of the river however, were in all probability washed down from lower impacted upstream habitats and may expectedly be able to again occupy habitats downstream if water quality and habitat availability improves. / Environmental Sciences / M. Sc. (Environmental Science)