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  • 1
    Keywords: Environmental management. ; Pollution. ; Environmental monitoring. ; Environmental Management. ; Pollution. ; Environmental Monitoring.
    Description / Table of Contents: Introduction -- Environmental background investigation of groundwater contamination sites -- Rating and evaluation of pollution source intensity for typical groundwater contamination sites -- Risk assessment of groundwater contamination sites -- Application case.
    Abstract: This book introduces readers to environmental background investigation, pollution source intensity evaluation and risk assessment approaches used at three main types of groundwater-contaminated sites: municipal domestic waste landfills, hazardous waste landfills and oil-contaminated sites. In addition, typical contaminated sites throughout China are examined to demonstrate how these approaches can be applied for their investigation, assessment and restoration. By reading this book, readers will gain a deeper understanding of the restoration and management of typical groundwater-contaminated sites.
    Type of Medium: Online Resource
    Pages: XI, 388 p. 145 illus., 115 illus. in color. , online resource.
    Edition: 1st ed. 2021.
    ISBN: 9789811528453
    DDC: 333.7
    Language: English
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  • 2
    Publication Date: 2023-03-08
    Keywords: Age, maximum/old; Age, minimum/young; Baoshan_Yangyi_Mine; China; Climate-Leaf Analysis Multivariate Program (CLAMP) (Wolfe, 1993); Coexistence Approach (Mosbrugger, V & Utescher, T, 1997); Epoch; Eryuan; Event label; Jianchuan; Longling_Daba_Mine; Mangdan; Mangdan_Coal_Mine; NECLIME; NECLIME_campaign; Neogene Climate Evolution in Eurasia; Paleontological sampling; PALSAMP; Precipitation, annual mean, maximum; Precipitation, annual mean, minimum; Precipitation, growing season; QU; Quarry; Sample code/label; Sample type; Standard error; Temperature, annual mean; Temperature, annual mean, maximum; Temperature, annual mean, minimum; Temperature, coldest month; Temperature, coldest month, maximum; Temperature, coldest month, minimum; Temperature, warmest month; Temperature, warmest month, maximum; Temperature, warmest month, minimum; Tengchong; Yunnan, China
    Type: Dataset
    Format: text/tab-separated-values, 112 data points
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  • 3
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    PANGAEA
    In:  Supplement to: Sun, Bai-Nian; Wu, Jing-Yu; Liu, Yu-Sheng Christopher; Ding, Su-Ting; Li, Xiang-Chuan; Xie, San-Ping; Yan, De-Fei; Lin, Zhi-Cheng (2011): Reconstructing Neogene vegetation and climates to infer tectonic uplift in western Yunnan, China. Palaeogeography, Palaeoclimatology, Palaeoecology, 304(3-4), 328-336, https://doi.org/10.1016/j.palaeo.2010.09.023
    Publication Date: 2023-01-13
    Description: Neogene climates and vegetation history of western Yunnan are reconstructed on the basis of known fossil plants using the Coexistence Approach (CA) and Leaf Margin Analysis (LMA). Four Neogene leaf floras from Tengchong, Jianchuan and Eryuan in southwestern China are analyzed by the CA, and the paleoclimatic data of one Miocene carpoflora from Longling and three Pliocene palynofloras from Longling, Yangyi and Eryuan are used for comparison. The Miocene vegetation of the whole of West Yunnan is subtropical evergreen broad-leaved forest, and a similar mean annual precipitation is inferred for Tengchong, Longling and Jianchuan. However, by the Late Pliocene a large difference in vegetation occurred between the two slopes of Gaoligong Mountain, western Yunnan. The region of Tengchong retained a subtropical evergreen broad-leaved forest vegetation, whereas in Yangyi and Eryuan a vertical vegetation zonation had developed, which consists, in ascending order, of humid evergreen broad-leaved, needle and broad-leaved mixed evergreen, and coniferous forests. Distinctively, the Late Pliocene vegetational patterns of West Yunnan were already very similar to those of the present, and the Pliocene mean annual precipitation in Tengchong was markedly higher than that of Yangyi and Eryuan. Considering that the overall vegetation of West Yunnan and the precipitation at Yangyi and Eryuan have undergone no distinct change since the Late Pliocene, we conclude that the Hengduan Mountains on the northern boundary of West Yunnan must have arisen after the Miocene and approached their highest elevation before the Late Pliocene. Furthermore, the fact of the eastern portion of the Tibetan Plateau underwent a slight uplift after the Late Pliocene is also supported.
    Keywords: Baoshan_Yangyi_Mine; China; Eryuan; Jianchuan; Longling_Daba_Mine; Mangdan; Mangdan_Coal_Mine; NECLIME; NECLIME_campaign; Neogene Climate Evolution in Eurasia; Paleontological sampling; PALSAMP; QU; Quarry; Tengchong; Yunnan, China
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 4
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    PANGAEA
    In:  Supplement to: Li, Xiang; Hu, Xiumian; Cai, Yuanfeng; Han, Zhiyan (2011): Quantitative analysis of iron oxide concentrations within Aptian-Albian cyclic oceanic red beds in ODP Hole 1049C, North Atlantic. Sedimentary Geology, 235(1-2), 91-99, https://doi.org/10.1016/j.sedgeo.2010.06.024
    Publication Date: 2024-01-09
    Description: Aptian–Albian sediments in Core 12X of Hole 1049C (ODP Leg 171B) are characterized by high-frequency cycles that consist of alternating layers of red and green/white clayey chalk, and claystone. The first derivative curves of diffuse reflectance spectra (DRS) for samples of different colors reveal that red (brown and orange) samples show clear peaks corresponding to hematite and goethite. Following treatment using the CBD (citrate-bicarbonate-dithionite) procedure, the red samples lost their red color and corresponding peaks in the first derivative curve, and became greenish or whitish. Therefore, hematite and goethite are the minerals responsible for the reddish change in sample color. However, these minerals behave differently from each other in terms of determining the color of sediment: hematite imparts a red color, whereas goethite imparts a yellow color. Therefore, a change in the proportions of hematite and goethite can cause a change in sediment color from orange to brown. To obtain the absolute contents of iron oxides in these sediments, we performed a quantitative analysis using DRS with multiple linear regression. The results reveal that the Albian brown beds contain 0.13–0.82% hematite (average value, 0.51%) and 0.22–0.81% goethite (average value, 0.58%). The Aptian orange beds contain 0.19–0.46% hematite (average value, 0.35%) and 0.29–0.67% goethite (average value, 0.50%). X-ray diffraction analysis of the Aptian and Albian cycles reveals no clear variations in mineral content with sediment color. It is suggested that hematite and goethite were derived from oxic environments during the period of deposition and early diagenesis. The oxic conditions were probably determined by the low accumulation rate of organic matter and the high content of dissolved oxygen in bottom water.
    Keywords: 171-1049C; Blake Nose, North Atlantic Ocean; Color reflectance interval 400-450 nm wavelength; Color reflectance interval 450-490 nm wavelength; Color reflectance interval 490-560 nm wavelength; Color reflectance interval 560-590 nm wavelength; Color reflectance interval 590-630 nm wavelength; Color reflectance interval 630-700 nm wavelength; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Goethite; Hematite, Fe2O3; Joides Resolution; Leg171B; Number; Ocean Drilling Program; ODP; Spectrophotometer Perkin-Elmer Lambda 6; X-ray diffraction (XRD)
    Type: Dataset
    Format: text/tab-separated-values, 189 data points
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  • 5
    Publication Date: 2024-03-06
    Keywords: Acer florinii; Acer paxii; Acer sp.; Age, maximum/old; Age, minimum/young; Alangium aequalifolium; Alnus sp.; Alseodaphne hainanensis; Berchemia miofloribunda; Berchemia yunnanensis; Betula mioluiminfera; Betula sp.; Calocedrus lantenoisii; Carpinus subcordata; Castanea miomollissima; Castanopsis sclerophylla; Castanopsis sp.; Celtis bungeana; China; Chukrasia sp.; Cinnamomum sp.; Cinnamomum subavenium; Cinnamomum tuantianensis; Cornus megaphylla; Cupressus sp.; Cyclea sp.; Cyclobalanopsis chevalieri; Cyclobalanopsis multiervis; Dioscorea sp.; Epoch; Eryuan; Event label; Evodia miosinica; Exbucklandia tengchongensis; Fagus sp.; Fossil determination; Fraxinus floribunda; Garcinia multiflora; Gymnocladus sp.; Heterosmilax yunnanensis; Ilex sp.; Jianchuan; Juglans sp.; Juglans tengchongensis; Lindera angustifolia; Lithocarpus lancifolius; Machilus leptophylla; Machilus longipedicellata; Machilus thunbergii; Magnolia sp.; Mahonia fortunei; Mallotus longifolius; Mallotus philippensis; Myrica esculenta; NECLIME; NECLIME_campaign; Neogene Climate Evolution in Eurasia; Nothaphoebe precavaleriei; ORDINAL NUMBER; Ormosia emarginata; Paleontological sampling; Paliurus sp.; PALSAMP; Phoebe megaphylla; Phoebe pseudoelanceolata; Phoebe pseudolanceolata; Phoebe sp.; Picea sp.; Pinus sp.; Pinus yunnanensis; Pistacia miochinensis; Populus sp.; Quercus aquifoliodes; Quercus gilliana; Quercus lianghensis; Quercus monimotricha; Quercus norini; Quercus pannosa; Quercus parachampionii; Quercus scottii; Quercus semicarpifolia; Quercus senescens; Quercus sp.; Quercus spathulata; Rhodoleia tengchongensis; Rhus miosuccedanea; Rhus trifolia; Robinia sp.; Sample code/label; Sassafras paratsumu; Smilax sp.; Syzygium buxifolium; Tengchong; Tilia miohenryana; Trapa sp.; Ulmus harutoriensis; Ulmus sp.; Viburnum ovalifolium; Zelkova ungeri
    Type: Dataset
    Format: text/tab-separated-values, 105 data points
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  • 6
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    PANGAEA
    In:  Supplement to: Zhao, Jinping; Li, Tao; Barber, David; Ren, Jingping; Pućko, Monika; Li, Shujiang; Li, Xiang (2010): Attenuation of lateral propagating light in sea ice measured with an artificial lamp in winter Arctic. Cold Regions Science and Technology, 61(1), 6-12, https://doi.org/10.1016/j.coldregions.2009.12.006
    Publication Date: 2023-12-13
    Description: The attenuation property of a lateral propagating light (LPL) in sea ice was measured using an artificial lamp in the Canadian Arctic during the 2007/2008 winter. A measurement method is proposed and applied whereby a recording instrument is buried in the sea ice and an artificial lamp is moved across the instrument. The apparent attenuation coefficient µ(lamda) for the lateral propagating light is obtained from the measured logarithmic relative variation rate. With the exception of blue and red lights, the attenuation coefficient changed little with wavelength, but changed considerably with depth. The vertical decrease of the attenuation coefficient was found to be correlated with salinity: the greater the salinity, the greater the attenuation coefficient. A clear linear relation of salinity and the lateral attenuation coefficient with R2 = 0.939 exists to address the close correlation of the attenuation of LPL with the scattering from the brine. The observed attenuation coefficient of LPL is much larger than that of the vertical propagation light, which we speculate to be caused by scattering. Part of this scattered component is transmitted out of the sea ice from the upper and lower surfaces.
    Keywords: Beaufort Sea; DEPTH, ice/snow; ICEM; Ice measurement; International Polar Year (2007-2008); ipy; IPY; Optical beam attenuation coefficient, 443 nm; Optical beam attenuation coefficient, 465 nm; Optical beam attenuation coefficient, 490 nm; Optical beam attenuation coefficient, 510 nm; Optical beam attenuation coefficient, 532 nm; Optical beam attenuation coefficient, 555 nm; Optical beam attenuation coefficient, 565 nm; Optical beam attenuation coefficient, 589 nm; Optical beam attenuation coefficient, 625 nm; Optical beam attenuation coefficient, 665 nm; Optical beam attenuation coefficient, 683 nm; Optical beam attenuation coefficient, 710 nm; Optical beam attenuation coefficient, 765 nm; Optical beam attenuation coefficient, 780 nm; Profiling Reflectance and Radiometer System PRR-810; Sample ID; SBeaufSea_D
    Type: Dataset
    Format: text/tab-separated-values, 210 data points
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  • 7
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    SPRINGER
    In:  EPIC3Climate Dynamics, SPRINGER, 53(9-10), pp. 5279-5291, ISSN: 0930-7575
    Publication Date: 2019-11-04
    Description: Atlantic water (AW) plays an important role in the thermal balance of the Arctic Ocean, but thus far there has been no comprehensive assessment of the AW layer in the Arctic Ocean simulated by coupled climate models in the framework of Coupled Model Intercomparison Project (CMIP). In this study we assessed the climatology and the trend of the Arctic AW layer in the historical simulations of 41 CMIP5 climate models. The results show that the CMIP5 intermodel spread is large in terms of simulated hydrography, AW core temperature (AWCT) and AW core depth (AWCD) in the Arctic Ocean. The CMIP5 multimodel means are found to be able to reproduce the main climatological spatial patterns of both the AWCT, which is warm near the Fram Strait and decreases along the AW pathways, and the AWCD, which deepens along the AW pathways. However, similar to standalone ocean-ice models, the CMIP5 climate models also face the common problems of too deep and too thick AW layer. AWCT bias in the Arctic Ocean is related to simulated water properties near the Fram Strait and in the Kara and Barents seas. Models with large AWCT biases are those with large biases in AW temperature in the Fram Strait. The biases of AWCT are also significantly correlated with the ocean temperature in the Kara Sea, which is modulated by winter cooling, hence the mixed layer depth and sea ice cover in the Barents Sea. The CMIP5 models largely underestimate the interannual variability of the AWCT, and the CMIP5-simulated increasing trend of the AWCT in the Arctic Ocean is considerably lower than the observed one since the late 1970s.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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  • 8
    Publication Date: 2022-05-26
    Description: © The Author(s), 2013. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Nature 500 (2013): 453–457, doi:10.1038/nature12326.
    Description: Loss of sexual reproduction is considered an evolutionary dead end for metazoans, but bdelloid rotifers challenge this view as they appear to have persisted asexually for millions of years1. Neither male sex organs nor meiosis have ever been observed in these microscopic animals: oocytes are formed through mitotic divisions, with no reduction of chromosome number and no indication of chromosome pairing2. However, current evidence does not exclude that they may engage in sex on rare, cryptic occasions. Here we report the genome of a bdelloid rotifer, Adineta vaga (Davis, 1873)3, and show that its structure is incompatible with conventional meiosis. At gene scale, the genome of A. vaga is tetraploid and comprises both anciently duplicated segments and less divergent allelic regions. However, in contrast to sexual species, the allelic regions are rearranged and sometimes even found on the same chromosome. Such structure does not allow meiotic pairing; instead, we find abundant evidence of gene conversion, which may limit the accumulation of deleterious mutations in the absence of meiosis. Gene families involved in resistance to oxidation, carbohydrate metabolism and defence against transposons are significantly expanded, which may explain why transposable elements cover only 3% of the assembled sequence. Furthermore, 8% of the genes are likely to be of non-metazoan origin and were probably acquired horizontally. This apparent convergence between bdelloids and prokaryotes sheds new light on the evolutionary significance of sex.
    Description: This work was supported by Genoscope-CES (where most of the sequencing was performed), by US National Science Foundation grants MCB-0821956 and MCB-1121334 to I.A., by German Research Foundation grant HA 5163/2-1 to O.H., by grant 11.G34.31.0008 fromthe Ministry of Education and Science of the Russian Federation to A.S.K., by grant NSF CAREER number 0644282 to M.K., by US National Science Foundation grant MCB-0923676 to D.B.M.W., by FRFC grant 2.4.655.09.F from the Belgian Fonds National de la Recherche Scientifique (FNRS) and a start-up grant from the University of Namur to K.V.D.; J.F.F. and K.V.D. thank also J.-P. Descy (University of Namur) for funding support.
    Repository Name: Woods Hole Open Access Server
    Type: Article
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  • 9
    Publication Date: 2022-10-20
    Description: Author Posting. © American Geophysical Union, 2021. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Geophysical Research Letters 48(19), (2021): e2021GL094364, https://doi.org/10.1029/2021GL094364.
    Description: The warm Gulf Stream sea surface temperatures strongly impact the evolution of winter clouds behind atmospheric cold fronts. Such cloud evolution remains challenging to model. The Gulf Stream is too wide within the ERA5 and MERRA2 reanalyses, affecting the turbulent surface fluxes. Known problems within the ERA5 boundary layer (too-dry and too-cool with too strong westerlies), ascertained primarily from ACTIVATE 2020 campaign aircraft dropsondes and secondarily from older buoy measurements, reinforce surface flux biases. In contrast, MERRA2 winter surface winds and air-sea temperature/humidity differences are slightly too weak, producing surface fluxes that are too low. Reanalyses boundary layer heights in the strongly forced winter cold-air-outbreak regime are realistic, whereas late-summer quiescent stable boundary layers are too shallow. Nevertheless, the reanalysis biases are small, and reanalyses adequately support their use for initializing higher-resolution cloud process modeling studies of cold-air outbreaks.
    Description: This work was supported by NASA grant 80NSSC19K0390 to ACTIVATE, a NASA Earth Venture Suborbital-3 (EVS-3) investigation funded by NASA's Earth Science Division and managed through the Earth System Science Pathfinder Program Office. The Pacific Northwest National Laboratory (PNNL) is operated for the US Department of Energy (DOE) by Battelle Memorial Institute under Contract DE-AC06-76RLO 1830.
    Description: 2022-03-08
    Keywords: Cold-air outbreaks ; Surface fluxes ; Gulf Stream ; ACTIVATE ; ERA5 ; MERRA2
    Repository Name: Woods Hole Open Access Server
    Type: Article
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  • 10
    Publication Date: 2022-08-19
    Description: © The Author(s), 2022. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Yuan, D., Yin, X., Li, X., Corvianawatie, C., Wang, Z., Li, Y., Yang, Y., Hu, X., Wang, J., Tan, S., Surinati, D., Purwandana, A., Wardana, A., Ismail, M., Budiman, A., Bayhaqi, A., Avianto, P., Santoso, P., Kusmanto, E., Dirhamsyah, Arifin, Z., & Pratt, L. A Maluku Sea intermediate western boundary current connecting Pacific Ocean circulation to the Indonesian Throughflow. Nature Communications, 13(1), (2022): 2093, https://doi.org/10.1038/s41467-022-29617-6.
    Description: The Indonesian Throughflow plays an important role in the global ocean circulation and climate. Existing studies of the Indonesian Throughflow have focused on the Makassar Strait and the exit straits, where the upper thermocline currents carry North Pacific waters to the Indian Ocean. Here we show, using mooring observations, that a previous unknown intermediate western boundary current (with the core at ~1000 m depth) exists in the Maluku Sea, which transports intermediate waters (primarily the Antarctic Intermediate Water) from the Pacific into the Seram-Banda Seas through the Lifamatola Passage above the bottom overflow. Our results suggest the importance of the western boundary current in global ocean intermediate circulation and overturn. We anticipate that our study is the beginning of more extensive investigations of the intermediate circulation of the Indo-Pacific ocean in global overturn, which shall improve our understanding of ocean heat and CO2 storages significantly.
    Description: This study is supported by NSFC (D.Y., Z.W., Y.L., Y.Y., S.T., J.W., and X.L.: 41720104008; D.Y., J.W., Y.L., X.L., Y.Y., S.T., X.H., and X.Y.: 91858204), the National Key Research and Development Program of China (D.Y. and X.L.: 2020YFA0608800), CAS (D.Y., Z.W., J.W., and Y.L.: XDB42000000), projects. Affiliations 1 and 2 share the first position. D.Y. is supported by QMSNL (2018SDKJ0104-02), and Shandong Provincial (U1606402) and the “Kunpeng Outstanding Scholar Program” of the FIO/NMR of China, J.W. supported by NSFC (41776011), Z.W. by NSFC (41876025).
    Repository Name: Woods Hole Open Access Server
    Type: Article
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