Connectivity of sediment transport in a semiarid environment: a synthesis for the Upper Jaguaribe Basin,Brazil

Purpose

Hydrosedimentological studies conducted in the semiarid Upper Jaguaribe Basin, Brazil, enabled the identification of the key processes controlling sediment connectivity at different spatial scales (10⁰–10⁴ km²).

Materials and methods

Water and sediment fluxes were assessed from discharge, sediment concentrations and reservoir siltation measurements. Additionally, mathematical modelling (WASA-SED model) was used to quantify water and sediment transfer within the watershed.

Results and discussion

Rainfall erosivity in the study area was moderate (4600 MJ mm ha^?1 h^?1 year^?1), whereas runoff depths (16–60 mm year^?1), and therefore the sediment transport capacity, were low. Consequently, ～60 % of the eroded sediment was deposited along the landscape, regardless of the spatial scale. The existing high-density reservoir network (contributing area of 6 km² per reservoir) also limits sediment propagation, retaining up to 47 % of the sediment at the large basin scale. The sediment delivery ratio (SDR) decreased with the spatial scale; on average, 41 % of the eroded sediment was yielded from the hillslopes, while for the whole 24,600-km² basin, the SDR was reduced to 1 % downstream of a large reservoir (1940-hm³ capacity).

Conclusions

Hydrological behaviour in the Upper Jaguaribe Basin represents a constraint on sediment propagation; low runoff depth is the main feature breaking sediment connectivity, which limits sediment transference from the hillslopes to the drainage system. Surface reservoirs are also important barriers, but their relative importance to sediment retention increases with scale, since larger contributing areas are more suitable for the construction of dams due to higher hydrological potential.     

Process-based modelling of erosion,sediment transport and reservoir siltation in mesoscale semi-arid catchments

Purpose

To support scientifically sound water management in dryland environments a modelling system has been developed for the quantitative assessment of water and sediment fluxes in catchments, transport in the river system, and retention in reservoirs. The spatial scale of interest is the mesoscale because this is the scale most relevant for management of water and land resources.

Materials and methods

This modelling system comprises process-oriented hydrological components tailored for dryland characteristics coupled with components comprising hillslope erosion, sediment transport and reservoir deposition processes. The spatial discretization is hierarchically designed according to a multi-scale concept to account for particular relevant process scales. The non-linear and partly intermittent run-off generation and sediment dynamics are dealt with by accounting for connectivity phenomena at the intersections of landscape compartments. The modelling system has been developed by means of data from nested research catchments in NE-Spain and in NE-Brazil.

Results and discussion

In the semi-arid NE of Brazil sediment retention along the topography is the main process for sediment retention at all scales, i.e. the sediment delivery is transport limited. This kind of deposition retains roughly 50 to 60 % of eroded sediment, maintaining a similar deposition proportion in all spatial scales investigated. On the other hand, the sediment retained in reservoirs is clearly related to the scale, increasing with catchment area. With increasing area, there are more reservoirs, increasing the possibility of deposition. Furthermore, the area increase also promotes an increase in flow volume, favouring the construction of larger reservoirs, which generally overflow less frequently and retain higher sediment fractions. The second example comprises a highly dynamic Mediterranean catchment in NE-Spain with nested sub-catchments and reveals the full dynamics of hydrological, erosion and deposition features. The run-off modelling performed well with only some overestimation during low-flow periods due to the neglect of water losses along the river. The simulated peaks in sediment flux are reproduced well, while low-flow sediment transport is less well captured, due to the disregard of sediment remobilization in the riverbed during low flow.

Conclusions

This combined observation and modelling study deepened the understanding of hydro-sedimentological systems characterized by flashy run-off generation and by erosion and sediment transport pulses through the different landscape compartments. The connectivity between the different landscape compartments plays a very relevant role, regarding both the total mass of water and sediment transport and the transport time through the catchment.     

How old are the eukaryotes?

Evidence from Precambrian sediments appears to indicate that nucleated (eukaryotic) organisms had become well established and relatively diverse about 850 +/- 100 million years ago and that eukaryotes were probably extant, and may have first appeared, as early as 1400 +/- 100 million years ago.     

Carbon isotopic studies of organic matter in precambrian rocks

Reduced carbon in early Precambrian cherts of the Fig Tree and upper and middle Onverwacht groups of South Africa is isotopically similar (the average value of delta(13)C(PDB) is -28.7 per mil) to photosynthetically produced organic matter of younger geological age. Reduced carbon in lower Onverwacht cherts (Theespruit formation) is anomalously heavy (the average value of delta(13)C(PDB) is -16.5 per mil). This discontinuity may reflect a major event in biological evolution.     

Artificial microfossils: experimental studies of permineralization of blue-green algae in silica

A technique has been developed to artificially fossilize microscopic algae in crystalline silica under conditions of moderately elevated temperature and pressure. The technique is designed to simulate geochemical processes thought to have resulted in the preservation of organic microfossils in Precambrian bedded cherts. In degree of preservation and mineralogic setting, the artificially permineralized microorganisms are comparable to naturally occurring fossil algae.     

Fecal Indicator and Pathogen Reduction in Vegetation Microcosms

Municipal wastewater has been applied as a fertilizer to coniferous forest in northern Sweden with the additional aims to purify the wastewater and reduce the treatment costs. This practice has the potential to introduce pathogenic microorganisms from the applied wastewater or sludge to the environment, with a subsequent risk of transmission to exposed humans or animals. Seasonality and climatological conditions, in particular low temperature, humidity and low sun intensity will furthermore affect the persistence of pathogens in the forest in northern Scandinavia and may therefore enhance the survival and thereby the exposure risk. The survival of two pathogens (Salmonella senftenberg and Campylobacter coli) and four fecal indicator organisms; bacteria strains (E. coli and E. fecalis) and bacteriophages (S. typhimurium phage 28 B and ?x174), used here as viral models, was evaluated in microcosms (60 Litre terrariums) with two vegetation regimes (characterized as moss and lichen) at selected temperatures (+3^?C to +27^?C) and artificial light exposure (light and dark). Salmonella persisted in high numbers after 35 days in the vegetation, indicating a potential risk for further transmission. Neither the vegetation regime nor temperature or light exposure as independent factors governed the reduction of the indicator bacteria and the bacteriophages. The persistence of the indicator organisms was generally best supported in the moss vegetation at low temperature in the dark, where the time for a 90% reduction (T₉₀) was in the range from 8 days (E. coli) to 31 days (Salmonella phage). The die-off characteristics found in this study provide baseline values for further validations in the field and verify that the purification and reuse of municipal wastewater in coniferous forest could potentially be responsible for transmission of fecal pathogens to humans and animals.     

Entwicklung und gestaltung gehölzreicher weidelandschaften auf reliefiertem niedermoor

Die drastische Reduzierung der Besatzstärke an Rindern auf 0,5–1 GV/ha LF nach der politischen Wende in Ostdeutschland schafft interessante Möglichkeiten der Neugestaltung von Weiden. Um stärker und gleichmäßiger wechselnde Aufenthaltsplätze in der Fläche zu induzieren, könnten Extensivweiden in einer Art aufgelockerter Parklandschaft gestaltet werden. Die Eignung verschiedener Baum‐ und Straucharten für Niedermoore wurde in der Forschungsstation Paulinenaue, nordwestlich von Berlin, analysiert.

Untersuchungen zeigten, daß zukünftig insbesondere ausländische Rinderrassen vor zu starker UV‐Belastung geschützt werden sollten. Die heutigen ausgeräumten Weidelandschaften bieten nicht genügend Schatten und auch nicht ausreichend Windund Wetterschutz während des Winters. Die Entwicklung von vielfältig strukturierten Weiden verbessert das Wohlbefinden der Tiere als auch die Biodiversität des gesamten Ökosystems. Die Landschaft gewinnt durch die Variation von Landschaftselementen, der Stoffkreislauf wird geregelter und die Akzeptanz für den ländlichen Raum in der Bevölkerung steigt.     

Implications of soil substrate and land use for properties of fen soils in North-East Germany Part III: Soil quality for grassland use

Abstract

The aim of the study was to analyse aspects of fen soil quality for grassland use with regard to the different topsoil structure and their status of earthification/moorshification (degradation). Fifty fens of different origin, structural status and land use intensity were sampled, analysed and scored by different methods: Visual Soil Assessment, Peerlkamp test and Muencheberg Soil Quality Rating. Suitable soil structure scores were found at different land use intensities with the exception of stock tracks on pastures. These had lower water and air permeability and lower soil strength. Highest visual scores of macrostructure were found where the water table was deeper; while highest overall soil quality scores occurred where the water table was optimum. The accelerated status of moorshification had no effect on the soil quality scores and on the crop yield. At lower levels of soil development (earthification) the crop yield was slightly lower due to higher proportions of inedible plants. It may be concluded that degraded peat soils will have no loss of soil quality and have relatively high soil quality for grassland use if the water table can be managed in a suitable range and the sward quality is maintained.     

The derivation of grassland vegetation types on the basis of site and land use characteristics

This study derives grassland communities from site, climate and land use characteristics, allowing yield estimation within the framework of model scenarios. Based on the dominant species, about 450 relevés, primarily of extensively used grassland from four regions of the North-East German lowlands, were classified into vegetation types using a cluster analysis. These types were then reclassified to known phytosociological communities. The relationship between the vegetational composition and the abiotic explanatory variables were verified by a discriminant analysis. The water supply level proved to be the most important factor influencing grassland vegetation. The impact of historical land use (especially the persistence of formerly sown species) reduced prognostic quality.