Nierenersatzverfahren – gestern, heute und morgen

Die Nierenersatztherapie ist eine der erfolgreichsten Geschichten eines künstlichen Organersatzes. Der vorliegende Artikel beschreibt die wichtigsten Schritte in der Evolution zur modernen Therapie mit Peritonealdialyse und Hämodialyse. Aktuelle Fragen im Bereich der Nierenersatztherapie werden diskutiert und zukünftige Entwicklungen aufgezeigt. Dem Patienten stehen heute diverse Therapiemöglichkeiten offen. Allerdings nur, wenn er mindestens ein halbes Jahr vor der Notwendigkeit eines Therapiebeginns die für ihn ideale Therapieform auswählen kann. Verspätete Zuweisungen und die Notwendigkeit eines akuten Dialysebeginns führen nicht nur zu einer erhöhten Mortalität, sondern auch dazu, dass eine präemptive Lebendnierentransplantation verunmöglicht wird. Zudem bleiben diese Patienten in der Regel im Dialysezentrum und können für eine Heimbehandlung, sei es nun in Form einer Peritonealdialyse oder Heimhämodialyse, nicht mehr motiviert werden.

The current and future state of interventional cardiology: a critical appraisal

After 75 years of invasive and over 50 years of interventional cardiology, cardiac catheter-based procedures have become the most frequently used interventions of modern medicine. Patients undergoing a percutaneous coronary intervention (PCI) outnumber those with coronary artery bypass surgery by a factor of 2 to 4. The default approach to PCI is the implantation of a (drug-eluting) stent, in spite of the fact that it improves the results of balloon angioplasty only in about 25% of cases. The dominance of stenting over conservative therapy or balloon angioplasty on one hand and bypass surgery on the other hand is a flagrant example of how medical research is digested an applied in real life. Apart from electrophysiological interventions, closure ot the patent foramen ovale and percutaneous replacement of the aortic valve in the elderly have the potential of becoming daily routine procedures in catheterization laboratories around the world. Stem cell regeneration of vessels or heart muscle, on the other hand, may remain a dream never to come true.

River loads and modern denudation of the Alps — A review

This paper presents the first comprehensive analysis of sediment and dissolved load across an entire mountain range. We investigate patterns and rates of modern denudation of the European Alps based on a compilation of data about river loads and reservoir sedimentation from 202 drainage basins that are between ca. 1 to 10,000 km2 large. The study basins cover about 50% of the total area of the Alps. Modern glaciated basins have the highest sediment yields of up to 7000 t km− 2 a− 1, which are on average 5 to 10 times higher than in non-glaciated basins. Likewise sediment yield and glacial cover are positively correlated. Instead, relief is a relatively weak predictor of sediment yield. The strong glacial impact in the correlations is due to glacier recession since the 19th century as well as due to glacial conditioning during repeated Quaternary glaciations which have produced the strong transient state of the Alpine landscape. We suggest that this is the major cause for ca. 3 fold enhanced denudation of the western compared to the eastern Alps. Chemical denudation rates are highest in the external Alps dominated by carbonate sedimentary rocks, where they make up about one third of total denudation. The high rates cannot be explained without anhydrite dissolution. We estimated that only 45% of the sediments mobilized in headwaters are exported out off the Alps, most sediments being trapped in artificial reservoirs. The total amount of sediment annually trapped within the Alps equates to 43 Mt. When corrected for sediment storage, we obtain an area-weighted mean total denudation rate for the Alps of about 0.32 mm a− 1. The pre-dam rate might be as high as 0.42 mm a− 1. In total, ca. 35 plus 23 Mt of mass are exported each year out of the Alps as solids and solutes, respectively. These rates are not enough to out pace modern rock uplift. Nevertheless, pattern of sediment yield across the Alps coincides roughly with the intensity of glacial conditioning and modern rock uplift, supporting the hypothesis of an erosion-driven uplift of the Alps.

Water versus ice: The competing roles of modern climate and Pleistocene glacial erosion in the Central Alps of Switzerland

Recent studies have identified relationships between landscape form, erosion and climate in regions of landscape rejuvenation, associated with increased denudation. Most of these landscapes are located in non-glaciated mountain ranges and are characterized by transient geomorphic features. The landscapes of the Swiss Alps are likewise in a transient geomorphic state as seen by multiple knickzones. In this mountain belt, the transient state has been related to erosional effects during the Late Glacial Maximum (LGM). Here, we focus on the catchment scale and categorize hillslopes based on erosional mechanisms, landscape form and landcover. We then explore relationships of these variables to precipitation and extent of LGM glaciers to disentangle modern versus palaeo controls on the modern shape of the Alpine landscape. We find that in grasslands, the downslope flux of material mainly involves unconsolidated material through hillslope creep, testifying a transport-limited erosional regime. Alternatively, strength-limited hillslopes, where erosion is driven by bedrock failure, are covered by forests and/or expose bedrock, and they display oversteepened hillslopes and channels. There, hillslope gradients and relief are more closely correlated with LGM ice occurrence than with precipitation or the erodibility of the underlying bedrock. We relate the spatial occurrence of the transport- and strength-limited process domains to the erosive effects of LGM glaciers. In particular, strength-limited, rock dominated basins are situated above the equilibrium line altitude (ELA) of the LGM, reflecting the ability of glaciers to scour the landscape beyond threshold slope conditions. In contrast, transport-limited, soil-mantled landscapes are common below the ELA. Hillslopes covered by forests occupy the elevations around the ELA and are constrained by the tree line. We conclude that the current erosional forces at work in the Central Alps are still responding to LGM glaciation, and that the modern climate has not yet impacted on the modern landscape.