TY - JOUR A1 - Zhang, Kai A1 - Chen, Zhiming A1 - Armin, Ardalan A1 - Dong, Sheng A1 - Xia, Ruoxi A1 - Yip, Hin-Lap A1 - Shoaee, Safa A1 - Huang, Fei A1 - Cao, Yong T1 - Efficient large area organic solar cells processed by blade-coating with single-component green solvent JF - Solar Rrl N2 - While the performance of laboratory-scale organic solar cells (OSCs) continues to grow, development of high efficiency large area OSCs remains a big challenge. Although a few attempts to produce large area organic solar cells (OSCs) have been reported, there are still challenges on the way to realizing efficient module devices, such as the low compatibility of the thickness-sensitive active layer with large area coating techniques, the frequent need for toxic solvents and tedious optimization processes used during device fabrication. In this work, highly efficient thickness-insensitive OSCs based on PTB7-Th:PC71BM that processed with single-component green solvent 2-methylanisole are presented, in which both junction thickness limitation and solvent toxicity issues are simultaneously addressed. Careful investigation reveals that this green solvent prevents the evolution of PC71BM into large area clusters resulting in reduced charge carrier recombination, and largely eliminates trapping centers, and thus improves the thickness tolerance of the films. These findings enable us to address the scalability and solvent toxicity issues and to fabricate a 16 cm(2) OSC with doctor-blade coating with a state-of-the-art power conversion efficiency of 7.5% using green solvent. KW - doctor-blade coating KW - green solvents KW - large area devices KW - organic solar cells KW - thickness insensitive active layers Y1 - 2017 U6 - https://doi.org/10.1002/solr.201700169 SN - 2367-198X VL - 2 IS - 1 PB - Wiley-VCH CY - Weinheim ER - TY - JOUR A1 - Wang, Rong A1 - Zhang, Yongzhan A1 - Wünnemann, Bernd A1 - Biskaborn, Boris A1 - Yin, He A1 - Xia, Fei A1 - Zhou, Lianfu A1 - Diekmann, Bernhard T1 - Linkages between Quaternary climate change and sedimentary processes in Hala Lake, northern Tibetan Plateau, China JF - Journal of Asian earth sciences N2 - Profundal lake sediment cores are often interpreted in line with diverse and detailed sedimentological processes to infer paleoenvironmental conditions. The effects of frozen lake surfaces on terrigenous sediment deposition and how climate changes on the Tibetan Plateau are reflected in these lakes, however, is seldom discussed. A lake sediment core from Hala Lake (590 km(2)), northeastern Tibetan Plateau spanning the time interval from the Last Glacial Maximum to the present was investigated using high-resolution grain-size composition of lacustrine deposits. Seismic analysis along a north-south profile across the lake was used to infer the sedimentary setting within the lake basin. Periods of freezing and melting processes on the lake surface were identified by MODIS (MOD10A1) satellite data. End-member modeling of the grain size distribution allowed the discrimination between lacustrine, eolian and fluvial sediments. The dominant clay sedimentation (slack water type) during the global Last Glacial Maximum (LGM) reflects ice interceptions in long cold periods, in contrast to abundant eolian input during abrupt cold events. Therefore, fluvial and slack water sedimentation processes can indicate changes in the local paleoclimate during periods of the lake being frozen, when eolian input was minor. Inferred warm (i.e., similar to 22.7 and 19.5 cal. ka BP) and cold (i.e., similar to 11-9 and 3-1.5 cal. ka BP) spells have significant environmental impacts, not only in the regional realm, but they are also coherent with global-scale climate events. The eolian input generally follows the trend of the mid-latitude westerly wind dynamics in winter, contributing medium-sized sand to the lake center, deposited within the ice cover during icing and melting phases. Enhanced input was dominant during the Younger Dryas, Heinrich Event 1 and at around 8.2 ka, equivalent to the well-known events of the North Atlantic realm. (C) 2015 Elsevier Ltd. All rights reserved. KW - Tibetan Plateau KW - Lake deposits KW - End-member modeling KW - Grain size KW - Pleistocene and Holocene climate Y1 - 2015 U6 - https://doi.org/10.1016/j.jseaes.2015.04.008 SN - 1367-9120 SN - 1878-5786 VL - 107 SP - 140 EP - 150 PB - Elsevier CY - Oxford ER -