HOW TO ASSURE THE MOST APPROPRIATE DOSAGE OF ANTIMICROBIAL DRUGS by Matjaž Pavlišič, Aleš Mrhar

“…On the</p><em><em></em></em><p align="LEFT">basis of the literature data we proposed markers to enhance</p><em><em></em></em><p align="LEFT">the prediction of clinical outcomes, e.g. time for which</p><em><em></em></em><p align="LEFT"><span style="font-family: GaramondItcTEE-LighItal; font-size: xx-small;"><span style="font-family: GaramondItcTEE-LighItal; font-size: xx-small;">drug plasma concentration exceeds MIC (t </span></span><span style="font-family: GaramondItcTEE-LighItal; font-size: xx-small;"><span style="font-family: GaramondItcTEE-LighItal; font-size: xx-small;">&gt; MIC</span></span><span style="font-family: GaramondItcTEE-LighItal; font-size: xx-small;"><span style="font-family: GaramondItcTEE-LighItal; font-size: xx-small;">), ratio between</span></span></p><em><em></em></em><p align="LEFT">peak plasma concentration of antimicrobial drug and MIC</p><em><em></em></em><p align="LEFT"><span style="font-family: GaramondItcTEE-LighItal; font-size: xx-small;"><span style="font-family: GaramondItcTEE-LighItal; font-size: xx-small;">(C</span></span><span style="font-family: GaramondItcTEE-LighItal; font-size: xx-small;"><span style="font-family: GaramondItcTEE-LighItal; font-size: xx-small;">max </span></span><span style="font-family: GaramondItcTEE-LighItal; font-size: xx-small;"><span style="font-family: GaramondItcTEE-LighItal; font-size: xx-small;">/MIC) and area under the inhibitory curve (AUIC).…”
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Water level variation at a beaver pond significantly impacts net CO₂ uptake of a continental bog by H. He, T. Moore, E. R. Humphreys, P. M. Lafleur, N. T. Roulet

“…<p>The carbon (<span class="inline-formula">C</span>) dynamics of northern peatlands are sensitive to hydrological changes owing to ecohydrological feedbacks. …”
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Past and future climate change effects on the thermal regime and oxygen solubility of four peri-alpine lakes by O. Desgué-Itier, L. Melo Vieira Soares, O. Anneville, D. Bouffard, D. Bouffard, V. Chanudet, P. A. Danis, P. A. Danis, I. Domaizon, J. Guillard, T. Mazure, N. Sharaf, N. Sharaf, F. Soulignac, V. Tran-Khac, B. Vinçon-Leite, J.-P. Jenny

“…Based on the shared socio-economic pathway SSP370 of the Intergovernmental Panel on Climate Change (IPCC), peri-alpine lakes could face an increase of 3.80 <span class="inline-formula">^∘</span>C (<span class="inline-formula">±0.20</span> <span class="inline-formula">^∘</span>C) in the next 70 years, accompanied by a decline of 1.0 mg L<span class="inline-formula">⁻¹</span> (<span class="inline-formula">±0.1</span> mg L<span class="inline-formula">⁻¹</span>) of <span class="inline-formula">O₂</span> solubility. …”
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Identifying and correcting interferences to PTR-ToF-MS measurements of isoprene and other urban volatile organic compounds by M. M. Coggon, C. E. Stockwell, C. E. Stockwell, M. S. Claflin, E. Y. Pfannerstill, L. Xu, L. Xu, L. Xu, J. B. Gilman, J. Marcantonio, C. Cao, K. Bates, K. Bates, G. I. Gkatzelis, A. Lamplugh, E. F. Katz, E. F. Katz, C. Arata, E. C. Apel, R. S. Hornbrook, F. Piel, F. Piel, F. Piel, F. Majluf, F. Majluf, D. R. Blake, A. Wisthaler, A. Wisthaler, M. Canagaratna, B. M. Lerner, A. H. Goldstein, A. H. Goldstein, J. E. Mak, C. Warneke

“…This study evaluates the extent to which fragmentation and other ionization processes impact urban measurements of the PTR-ToF-MS ions typically assigned to isoprene (<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M1" display="inline" overflow="scroll" dspmath="mathml"><mrow><mi>m</mi><mo>/</mo><mi>z</mi></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="23pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="91270dba487782af7360c80516416e4b"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="amt-17-801-2024-ie00001.svg" width="23pt" height="14pt" src="amt-17-801-2024-ie00001.png"/></svg:svg></span></span> 69, C<span class="inline-formula">₅</span>H<span class="inline-formula">₈</span>H<span class="inline-formula">⁺</span>), acetaldehyde (<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M5" display="inline" overflow="scroll" dspmath="mathml"><mrow><mi>m</mi><mo>/</mo><mi>z</mi></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="23pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="46f32566b65c77f385ccc58250dc589d"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="amt-17-801-2024-ie00002.svg" width="23pt" height="14pt" src="amt-17-801-2024-ie00002.png"/></svg:svg></span></span> 45, CH<span class="inline-formula">₃</span>CHO<span class="inline-formula">⁺</span>), and benzene (<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M8" display="inline" overflow="scroll" dspmath="mathml"><mrow><mi>m</mi><mo>/</mo><mi>z</mi></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="23pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="d93d3cda2a0fb8602765a5ab31f8bec1"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="amt-17-801-2024-ie00003.svg" width="23pt" height="14pt" src="amt-17-801-2024-ie00003.png"/></svg:svg></span></span> 79, C<span class="inline-formula">₆</span>H<span class="inline-formula">₆</span>H<span class="inline-formula">⁺</span>). …”
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Spatial and temporal variation in <i>δ</i>¹³C values of methane emitted from a hemiboreal mire: methanogenesis, methanotrophy, and hysteresis by J. Rinne, J. Rinne, P. Łakomiec, P. Vestin, J. D. White, P. Weslien, J. Kelly, N. Kljun, L. Ström, L. Klemedtsson

“…According to the spatial <span class="inline-formula"><i>δ</i>¹³</span>C–<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M11" display="inline" overflow="scroll" dspmath="mathml"><mrow><msub><mi>F</mi><mrow class="chem"><msub><mi mathvariant="normal">CH</mi><mn mathvariant="normal">4</mn></msub></mrow></msub></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="23pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="91e8853d44f64a0711d31d2192a7eb30"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="bg-19-4331-2022-ie00002.svg" width="23pt" height="14pt" src="bg-19-4331-2022-ie00002.png"/></svg:svg></span></span> relations, methanotrophy was unlikely to be the dominating cause for the spatial variation. …”
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Impacts of water partitioning and polarity of organic compounds on secondary organic aerosol over eastern China by J. Li, J. Li, H. Zhang, Q. Ying, Z. Wu, Z. Wu, Y. Zhang, Y. Zhang, X. Wang, X. Wang, X. Wang, X. Li, Y. Sun, M. Hu, M. Hu, Y. Zhang, Y. Zhang, J. Hu, J. Hu

“…The correlation of <span class="inline-formula"><i>κ</i></span> with the <span class="inline-formula">O:C</span> ratio varies significantly across different cities and seasons. …”
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Modelling the terrestrial nitrogen and phosphorus cycle in the UVic ESCM by M. L. De Sisto, M. L. De Sisto, A. H. MacDougall, N. Mengis, S. Antoniello

“…<span class="inline-formula">CNP</span> simulation resulted in a reduction of 11 % of the mean GPP and a reduction of 23 % of the vegetation biomass compared to the baseline <span class="inline-formula">C</span> simulation. These results are in better agreement with observations, particularly in tropical regions where <span class="inline-formula">P</span> limitation is known to be important. …”
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Local-to-regional methane emissions from the Upper Silesian Coal Basin (USCB) quantified using UAV-based atmospheric measurements by T. Andersen, Z. Zhao, M. de Vries, J. Necki, J. Swolkien, M. Menoud, T. Röckmann, A. Roiger, A. Fix, W. Peters, W. Peters, H. Chen, H. Chen

“…In addition, we also measured <span class="inline-formula"><i>δ</i>¹³C</span>-<span class="inline-formula">CH₄</span>, <span class="inline-formula"><i>δ</i>²H</span>-<span class="inline-formula">CH₄</span>, ambient temperature, pressure, relative humidity, surface wind speed, and surface wind direction. …”
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Organic matter characteristics of a rapidly eroding permafrost cliff in NE Siberia (Lena Delta, Laptev Sea region) by C. Haugk, C. Haugk, C. Haugk, L. L. Jongejans, L. L. Jongejans, K. Mangelsdorf, M. Fuchs, O. Ogneva, O. Ogneva, O. Ogneva, J. Palmtag, J. Palmtag, G. Mollenhauer, G. Mollenhauer, P. J. Mann, P. P. Overduin, G. Grosse, G. Grosse, T. Sanders, R. E. Tuerena, L. Schirrmeister, S. Wetterich, S. Wetterich, A. Kizyakov, C. Karger, J. Strauss

“…The elevated ratio of iso- and anteiso-branched fatty acids (FAs) relative to mid- and long-chain (C <span class="inline-formula">≥</span> 20) <span class="inline-formula"><i>n</i></span>-FAs in the interstadial MIS 3 and the interglacial MIS 1 deposits suggests stronger microbial activity and consequently higher input of bacterial biomass during these climatically warmer periods. …”
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Unambiguous identification of N-containing oxygenated organic molecules using a chemical-ionization Orbitrap (CI-Orbitrap) in an eastern Chinese megacity by Y. Lu, Y. Lu, Y. Ma, D. D. Huang, S. Lou, S. Jing, Y. Gao, H. Wang, Y. Zhang, H. Chen, Y. Chang, N. Yan, J. Chen, C. George, M. Riva, C. Huang

“…The 2N-OOM<span class="inline-formula">_Ali</span> was the most abundant 2N-OOM, and its fraction even increased on the polluted day with an enhanced proportion of the ones with nC <span class="inline-formula"><i>&gt;</i>10</span>. …”
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<i>δ</i>¹³C, CO₂&thinsp;∕&thinsp;³He and ³He&thinsp;∕&thinsp;⁴He ratios reveal the presence of mantle gas in the CO<sub>2</su... by A. Defourny, A. Defourny, P.-H. Blard, P.-H. Blard, L. Zimmermann, P. Jobé, A. Collignon, F. Nguyen, A. Dassargues

“…The combination of <span class="inline-formula"><i>δ</i>¹³C</span> (between ca. <span class="inline-formula">−9 ‰</span> VPDB<span class="note-anchor" id="fna_Ch1.Footn1"><a href="#fn_Ch1.Footn1">¹</a></span> and <span class="inline-formula">−2 ‰</span> VPDB), <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M19" display="inline" overflow="scroll" dspmath="mathml"><mrow class="chem"><msub><mi mathvariant="normal">CO</mi><mn mathvariant="normal">2</mn></msub><msup><mo>/</mo><mn mathvariant="normal">3</mn></msup><mi mathvariant="normal">He</mi></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="48pt" height="16pt" class="svg-formula" dspmath="mathimg" md5hash="f571d99770c11306333b27ed5ca30b11"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="hess-26-2637-2022-ie00009.svg" width="48pt" height="16pt" src="hess-26-2637-2022-ie00009.png"/></svg:svg></span></span> ratio (between <span class="inline-formula">1.9×10⁸</span> and <span class="inline-formula">2.9×10⁹</span>) and <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M22" display="inline" overflow="scroll" dspmath="mathml"><mrow class="chem"><msup><mi/><mn mathvariant="normal">3</mn></msup><mi mathvariant="normal">He</mi><msup><mo>/</mo><mn mathvariant="normal">4</mn></msup><mi mathvariant="normal">He</mi></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="46pt" height="15pt" class="svg-formula" dspmath="mathimg" md5hash="5e8bb6b618862902b1a0e7bf75a65b08"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="hess-26-2637-2022-ie00010.svg" width="46pt" height="15pt" src="hess-26-2637-2022-ie00010.png"/></svg:svg></span></span> (between 0.92 and 2.70 Ra) shows with a high level of confidence that the <span class="inline-formula">CO₂</span> in the carbogaseous groundwater of Spa and Bru has a mantle origin. …”
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Fe-bearing vanadium dioxide–paramontroseite: structural details and high-temperature transformation by N. Curetti, A. Pavese

“…Thermal expansion is anisotropic, leading to the following <span class="inline-formula"><i>β</i></span> coefficients: <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M15" display="inline" overflow="scroll" dspmath="mathml"><mrow><mo>-</mo><mn mathvariant="normal">2.0</mn><mo>×</mo><msup><mn mathvariant="normal">10</mn><mrow><mo>-</mo><mn mathvariant="normal">5</mn></mrow></msup></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="59pt" height="13pt" class="svg-formula" dspmath="mathimg" md5hash="4dfc02a6053a4294b6cbe98cdc222976"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="ejm-35-373-2023-ie00001.svg" width="59pt" height="13pt" src="ejm-35-373-2023-ie00001.png"/></svg:svg></span></span>, <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M16" display="inline" overflow="scroll" dspmath="mathml"><mrow><mn mathvariant="normal">3.0</mn><mo>×</mo><msup><mn mathvariant="normal">10</mn><mrow><mo>-</mo><mn mathvariant="normal">5</mn></mrow></msup></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="51pt" height="13pt" class="svg-formula" dspmath="mathimg" md5hash="8cc417b3ec8f921814a72838e9c03d99"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="ejm-35-373-2023-ie00002.svg" width="51pt" height="13pt" src="ejm-35-373-2023-ie00002.png"/></svg:svg></span></span>, <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M17" display="inline" overflow="scroll" dspmath="mathml"><mrow><mn mathvariant="normal">0.8</mn><mo>×</mo><msup><mn mathvariant="normal">10</mn><mrow><mo>-</mo><mn mathvariant="normal">5</mn></mrow></msup></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="51pt" height="13pt" class="svg-formula" dspmath="mathimg" md5hash="1e2705fa2131d85215d6eed4c0d0304c"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="ejm-35-373-2023-ie00003.svg" width="51pt" height="13pt" src="ejm-35-373-2023-ie00003.png"/></svg:svg></span></span> and <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M18" display="inline" overflow="scroll" dspmath="mathml"><mrow><mn mathvariant="normal">1.8</mn><mo>×</mo><msup><mn mathvariant="normal">10</mn><mrow><mo>-</mo><mn mathvariant="normal">5</mn></mrow></msup></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="51pt" height="13pt" class="svg-formula" dspmath="mathimg" md5hash="5851cc401e05a481a4c4a46ee741295c"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="ejm-35-373-2023-ie00004.svg" width="51pt" height="13pt" src="ejm-35-373-2023-ie00004.png"/></svg:svg></span></span> <span class="inline-formula">^∘</span>C<span class="inline-formula">⁻¹</span> for <span class="inline-formula"><i>a</i></span>, <span class="inline-formula"><i>b</i></span>, <span class="inline-formula"><i>c</i></span> and <span class="inline-formula"><i>V</i></span>, respectively. …”
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Tunnelled central venous catheter-related bloodstream infection in Canadian blood stem cell transplant recipients: Associated costs by Melanie Keeler, Barbara K. Haas, Michael Nieswiadomy, Charles McConnel, Sally Northam, Lynn Savoie

“…</em></p><p class="p1"><strong>K</strong><span class="s1"><strong>ey </strong></span><strong>words:</strong> c<span class="s1">atheter related b</span>loodstr<span class="s1">ea</span>m<span class="s1"> in</span>f<span class="s1">ec</span>t<span class="s1">i</span>on,cost,<span class="s1"> s</span>tem c<span class="s1">e</span>llt<span class="s1">ra</span>nspl<span class="s1">a</span>nt</p>…”
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Distinct diurnal variation in organic aerosol hygroscopicity and its relationship with oxygenated organic aerosol by Y. Kuang, Y. He, W. Xu, P. Zhao, Y. Cheng, G. Zhao, J. Tao, N. Ma, H. Su, Y. Zhang, J. Sun, P. Cheng, W. Yang, S. Zhang, C. Wu, Y. Sun, C. Zhao

“…The derived <span class="inline-formula"><i>κ</i>_OA</span> was highly correlated with <span class="inline-formula"><i>f</i>₄₄</span> (fraction of <span class="inline-formula"><i>m</i>∕<i>z</i></span> 44 in OA measured by CV-ToF-ACSM), an indicator of the oxidation degree of OA (<span class="inline-formula"><i>R</i>=0.79</span>), and the relationship can be parameterized as <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M17" display="inline" overflow="scroll" dspmath="mathml"><mrow><msub><mi mathvariant="italic">κ</mi><mi mathvariant="normal">OA</mi></msub><mo>=</mo><mn mathvariant="normal">1.04</mn><mo>×</mo><msub><mi>f</mi><mn mathvariant="normal">44</mn></msub><mo>-</mo><mn mathvariant="normal">0.02</mn></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="111pt" height="12pt" class="svg-formula" dspmath="mathimg" md5hash="9890895a6671a6bb2a4f1ad14f52e15a"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="acp-20-865-2020-ie00001.svg" width="111pt" height="12pt" src="acp-20-865-2020-ie00001.png"/></svg:svg></span></span> (<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M18" display="inline" overflow="scroll" dspmath="mathml"><mrow><msub><mi mathvariant="italic">κ</mi><mi mathvariant="normal">OA</mi></msub><mo>=</mo><mn mathvariant="normal">0.3</mn><mo>×</mo><mrow class="chem"><mi mathvariant="normal">O</mi><mo>:</mo><mi mathvariant="normal">C</mi></mrow><mo>-</mo><mn mathvariant="normal">0.02</mn></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="116pt" height="13pt" class="svg-formula" dspmath="mathimg" md5hash="0c7ee3d913682589678ebfbabba540ac"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="acp-20-865-2020-ie00002.svg" width="116pt" height="13pt" src="acp-20-865-2020-ie00002.png"/></svg:svg></span></span>, based on the relationship between the <span class="inline-formula"><i>f</i>₄₄</span> and <span class="inline-formula">O∕C</span> ratio for CV-ToF-ACSM). On average, <span class="inline-formula"><i>κ</i>_OA</span> reached the minimum (0.02) in the morning near 07:30 local time (LT) and then increased rapidly, reaching the peak value of 0.16 near 14:30&thinsp;LT. …”
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Contributions of biomass-burning, urban, and biogenic emissions to the concentrations and light-absorbing properties of particulate matter in central Amazonia during the dry season by S. S. de Sá, L. V. Rizzo, B. B. Palm, B. B. Palm, P. Campuzano-Jost, D. A. Day, L. D. Yee, R. Wernis, G. Isaacman-VanWertz, G. Isaacman-VanWertz, J. Brito, J. Brito, S. Carbone, S. Carbone, Y. J. Liu, Y. J. Liu, A. Sedlacek, S. Springston, A. H. Goldstein, H. M. J. Barbosa, M. L. Alexander, P. Artaxo, J. L. Jimenez, S. T. Martin, S. T. Martin

“…A decrease in <span class="inline-formula"><i>b</i>_abs,BrC</span> was observed as the mass concentration of nitrogen-containing organic compounds decreased and the organic PM<span class="inline-formula">₁</span> <span class="inline-formula">O:C</span> ratio increased, suggesting atmospheric bleaching of the BrC components. …”
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Climate signals in stable carbon and hydrogen isotopes of lignin methoxy groups from southern German beech trees by A. Wieland, M. Greule, P. Roemer, J. Esper, J. Esper, F. Keppler, F. Keppler

“…Initial <span class="inline-formula"><i>δ</i>¹³C_LM</span> values were corrected for the Suess effect (a decrease of <span class="inline-formula"><i>δ</i>¹³C</span> in atmospheric CO<span class="inline-formula">₂</span>) and physiological tree responses to increasing atmospheric CO<span class="inline-formula">₂</span> concentrations considering a range of published discrimination factors. …”
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Highest methane concentrations in an Arctic river linked to local terrestrial inputs by K. Castro-Morales, A. Canning, S. Arzberger, W. A. Overholt, K. Küsel, K. Küsel, O. Kolle, M. Göckede, N. Zimov, A. Körtzinger, A. Körtzinger

“…These key sites were characterized by warm waters (<span class="inline-formula"><i>T</i>&gt;14.5</span> <span class="inline-formula">^∘C</span>) and low specific conductivities (<span class="inline-formula"><i>κ</i>&lt;88</span> <span class="inline-formula">µS cm⁻¹</span>). …”
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Global datasets of hourly carbon and water fluxes simulated using a satellite-based process model with dynamic parameterizations by J. Leng, J. M. Chen, W. Li, X. Luo, M. Xu, J. Liu, R. Wang, C. Rogers, B. Li, Y. Yan

“…However, these models often estimate GPP and ET at coarse daily or monthly steps, hindering analysis of ecosystem dynamics at the diurnal (hourly) scales, and prescribe some essential parameters (i.e., the Ball–Berry slope (<span class="inline-formula"><i>m</i></span>) and the maximum carboxylation rate at 25 °C (<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M2" display="inline" overflow="scroll" dspmath="mathml"><mrow><msubsup><mi>V</mi><mi mathvariant="normal">cmax</mi><mn mathvariant="normal">25</mn></msubsup></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="27pt" height="16pt" class="svg-formula" dspmath="mathimg" md5hash="6843e2ad912be589c7d614809a188ea9"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="essd-16-1283-2024-ie00001.svg" width="27pt" height="16pt" src="essd-16-1283-2024-ie00001.png"/></svg:svg></span></span>)) as constant, inducing uncertainties in the estimates of GPP and ET. …”
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Johan Galtung, el devenir Histórico como proyecto existencial by Percy Calderón Concha

“…<p><span>E</span><span>l</span><span> </span><span>2009</span><span> </span><span>r</span><span>eco</span><span>r</span><span>damos</span><span> </span><span>los</span><span> </span><span>50</span><span> </span><span>años</span><span> </span><span>de</span><span> </span><span>la</span><span> </span><span>c</span><span>r</span><span>eación</span><span> </span><span>del</span><span> </span><span><em>I</em></span><span><em>nte</em></span><span><em>r</em></span><span><em>national</em></span><span><em> </em></span><span><em>P</em></span><span><em>eace</em></span><span><em> </em></span><span><em>R</em></span><span><em>esea</em></span><span><em>r</em></span><span><em>ch</em></span><span><em> </em></span><span><em>I</em></span><span><em>stitute </em></span><span><em>o</em></span><em>f</em><span><em> </em></span><span><em>Osl</em></span><em>o</em><span><em> </em></span><span>(IPRIO</span>)<span> </span>a<span> </span><span>iniciativ</span>a<span> </span><span>de</span>l<span> </span><span>matemátic</span>o<span> </span>y<span> </span><span>sociólog</span>o<span> </span><span>no</span><span>r</span><span>ueg</span>o<span> </span><span>J</span><span>oha</span>n<span> </span><span>Galtung</span>.…”
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Heterogeneity and chemical reactivity of the remote troposphere defined by aircraft measurements – corrected by H. Guo, C. M. Flynn, M. J. Prather, S. A. Strode, S. D. Steenrod, L. Emmons, F. Lacey, F. Lacey, J.-F. Lamarque, A. M. Fiore, G. Correa, L. T. Murray, G. M. Wolfe, G. M. Wolfe, J. M. St. Clair, J. M. St. Clair, M. Kim, J. Crounse, G. Diskin, J. DiGangi, B. C. Daube, B. C. Daube, R. Commane, R. Commane, K. McKain, K. McKain, J. Peischl, J. Peischl, T. B. Ryerson, T. B. Ryerson, C. Thompson, T. F. Hanisco, D. Blake, N. J. Blake, E. C. Apel, R. S. Hornbrook, J. W. Elkins, E. J. Hintsa, E. J. Hintsa, F. L. Moore, F. L. Moore, S. C. Wofsy

“…In this paper we present and analyze a data set of 10 s (2 km) merged and gap-filled observations of the key reactive species driving the chemical budgets of O<span class="inline-formula">₃</span> and CH<span class="inline-formula">₄</span> (O<span class="inline-formula">₃</span>, CH<span class="inline-formula">₄</span>, CO, H<span class="inline-formula">₂</span>O, HCHO, H<span class="inline-formula">₂</span>O<span class="inline-formula">₂</span>, CH<span class="inline-formula">₃</span>OOH, C<span class="inline-formula">₂</span>H<span class="inline-formula">₆</span>, higher alkanes, alkenes, aromatics, NO<span class="inline-formula">_<i>x</i></span>, HNO<span class="inline-formula">₃</span>, HNO<span class="inline-formula">₄</span>, peroxyacetyl nitrate, and other organic nitrates), consisting of 146 494 distinct air parcels from ATom deployments 1 through 4. …”
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