TY - JOUR A1 - Hawro, Tomasz A1 - Przybylowicz, Katarzyna A1 - Spindler, Max A1 - Hawro, Marlena A1 - Steć, Michał A1 - Altrichter, Sabine A1 - Weller, Karsten A1 - Magerl, Markus A1 - Reidel, Ulrich A1 - Alarbeed, Ezzat A1 - Alraboni, Ola A1 - Maurer, Marcus A1 - Metz, Martin T1 - The characteristics and impact of pruritus in adult dermatology patients BT - a prospective, cross-sectional study JF - Journal of the American Academy of Dermatology N2 - Background: Pruritus often accompanies chronic skin diseases, exerting considerable burden on many areas of patient functioning; this burden and the features of pruritus remain insufficiently characterized. Objective: To investigate characteristics, including localization patterns, and burden of pruritus in patients with chronic dermatoses. Methods: We recruited 800 patients with active chronic skin diseases. We assessed pruritus intensity, localization, and further characteristics. We used validated questionnaires to assess quality of life, work productivity and activity impairment, anxiety, depression, and sleep quality. Results: Nine out of every 10 patients had experienced pruritus throughout their disease and 73% in the last 7 days. Pruritus often affected the entire body and was not restricted to skin lesions. Patients with moderate to severe pruritus reported significantly more impairment to their sleep quality and work productivity, and they were more depressed and anxious than control individuals and patients with mild or no pruritus. Suicidal ideations were highly prevalent in patients with chronic pruritus (18.5%) and atopic dermatitis (11.8%). Conclusions: Pruritus prevalence and intensity are very high across all dermatoses studied; intensity is linked to impairment in many areas of daily functioning. Effective treatment strategies are urgently required to treat pruritus and the underlying skin disease. ( J Am Acad Dermatol 2021;84:691-700.) KW - activity KW - anxiety KW - depression KW - pruritus KW - quality of life KW - sleep quality KW - suicidal ideations KW - work productivity Y1 - 2021 U6 - https://doi.org/10.1016/J.JAAD.2020.08.035 SN - 0190-9622 SN - 1097-6787 VL - 84 IS - 3 SP - 691 EP - 700 PB - Elsevier CY - Amsterdam [u.a.] ER - TY - JOUR A1 - Moradi, Ahmad B. A1 - Carminati, Andrea A1 - Vetterlein, Doris A1 - Vontobel, Peter A1 - Lehmann, Eberhard A1 - Weller, Ulrich A1 - Hopmans, Jan W. A1 - Vogel, Hans-Jörg A1 - Oswald, Sascha T1 - Three-dimensional visualization and quantification of water content in the rhizosphere JF - New phytologist : international journal of plant science N2 - Despite the importance of rhizosphere properties for water flow from soil to roots, there is limited quantitative information on the distribution of water in the rhizosphere of plants. Here, we used neutron tomography to quantify and visualize the water content in the rhizosphere of the plant species chickpea (Cicer arietinum), white lupin (Lupinus albus), and maize (Zea mays) 12 d after planting. We clearly observed increasing soil water contents (h) towards the root surface for all three plant species, as opposed to the usual assumption of decreasing water content. This was true for tap roots and lateral roots of both upper and lower parts of the root system. Furthermore, water gradients around the lower part of the roots were smaller and extended further into bulk soil compared with the upper part, where the gradients in water content were steeper. Incorporating the hydraulic conductivity and water retention parameters of the rhizosphere into our model, we could simulate the gradual changes of h towards the root surface, in agreement with the observations. The modelling result suggests that roots in their rhizosphere may modify the hydraulic properties of soil in a way that improves uptake under dry conditions. KW - extent of rhizosphere KW - modelling KW - neutron tomography KW - rhizosphere hydraulic properties KW - root water uptake KW - soil moisture profile KW - water distribution Y1 - 2011 U6 - https://doi.org/10.1111/j.1469-8137.2011.03826.x SN - 0028-646X VL - 192 IS - 3 SP - 653 EP - 663 PB - Wiley-Blackwell CY - Hoboken ER - TY - JOUR A1 - Carminati, Andrea A1 - Schneider, Christoph L. A1 - Moradi, Ahmad B. A1 - Zarebanadkouki, Mohsen A1 - Vetterlein, Doris A1 - Vogel, Hans-Jörg A1 - Hildebrandt, Anke A1 - Weller, Ulrich A1 - Schüler, Lennart A1 - Oswald, Sascha T1 - How the rhizosphere may favor water availability to roots JF - Vadose zone journal N2 - Recent studies have shown that rhizosphere hydraulic properties may differ from those of the bulk soil. Specifically, mucilage at the root-soil interface may increase the rhizosphere water holding capacity and hydraulic conductivity during drying. The goal of this study was to point out the implications of such altered rhizosphere hydraulic properties for soil-plant water relations. We addressed this problem through modeling based on a steady-rate approach. We calculated the water flow toward a single root assuming that the rhizosphere and bulk soil were two concentric cylinders having different hydraulic properties. Based on our previous experimental results, we assumed that the rhizosphere had higher water holding capacity and unsaturated conductivity than the bulk soil. The results showed that the water potential gradients in the rhizosphere were much smaller than in the bulk soil. The consequence is that the rhizosphere attenuated and delayed the drop in water potential in the vicinity of the root surface when the soil dried. This led to increased water availability to plants, as well as to higher effective conductivity under unsaturated conditions. The reasons were two: (i) thanks to the high unsaturated conductivity of the rhizosphere, the radius of water uptake was extended from the root to the rhizosphere surface; and (ii) thanks to the high soil water capacity of the rhizosphere, the water depletion in the bulk soil was compensated by water depletion in the rhizosphere. We conclude that under the assumed conditions, the rhizosphere works as an optimal hydraulic conductor and as a reservoir of water that can be taken up when water in the bulk soil becomes limiting. Y1 - 2011 U6 - https://doi.org/10.2136/vzj2010.0113 SN - 1539-1663 VL - 10 IS - 3 SP - 988 EP - 998 PB - Soil Science Society of America CY - Madison ER -