Syngas production and applications for greenhouse gas mitigation by Amin, N. S., Tahir, M.

Survival probabilities of atmospheric particles: comparison based on theory, cluster population simulations, and observations in Beijing by S. Tuovinen, R. Cai, V.-M. Kerminen, J. Jiang, C. Yan, C. Yan, M. Kulmala, J. Kontkanen, J. Kontkanen

“…In this study, we investigate and compare survival probabilities from 1.5 to 3 nm (<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M1" display="inline" overflow="scroll" dspmath="mathml"><mrow><msub><mi>J</mi><mn mathvariant="normal">3</mn></msub><mo>/</mo><msub><mi>J</mi><mn mathvariant="normal">1.5</mn></msub></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="36pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="dd965924e58000091851a6e4ed477e28"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="acp-22-15071-2022-ie00001.svg" width="36pt" height="14pt" src="acp-22-15071-2022-ie00001.png"/></svg:svg></span></span>), from 3 to 6 nm (<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M2" display="inline" overflow="scroll" dspmath="mathml"><mrow><msub><mi>J</mi><mn mathvariant="normal">6</mn></msub><mo>/</mo><msub><mi>J</mi><mn mathvariant="normal">3</mn></msub></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="29pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="1eaddf744c9d5dd53aebbecd0288f323"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="acp-22-15071-2022-ie00002.svg" width="29pt" height="14pt" src="acp-22-15071-2022-ie00002.png"/></svg:svg></span></span>), and from 6 to 10 nm (<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M3" display="inline" overflow="scroll" dspmath="mathml"><mrow><msub><mi>J</mi><mn mathvariant="normal">10</mn></msub><mo>/</mo><msub><mi>J</mi><mn mathvariant="normal">6</mn></msub></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="34pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="49d86c438e0c64b85c142a1ab456cbde"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="acp-22-15071-2022-ie00003.svg" width="34pt" height="14pt" src="acp-22-15071-2022-ie00003.png"/></svg:svg></span></span>) based on analytical formulae, cluster population simulations, and atmospheric observations from Beijing. …”
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Drivers of rapid geomagnetic variations at high latitudes by L. Juusola, A. Viljanen, A. P. Dimmock, M. Kellinsalmi, A. Schillings, J. M. Weygand

“…While the most intense external <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M4" display="inline" overflow="scroll" dspmath="mathml"><mrow><mo>|</mo><mi mathvariant="normal">d</mi><mi mathvariant="bold-italic">H</mi><mo>/</mo><mi mathvariant="normal">d</mi><mi>t</mi><mo>|</mo></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="40pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="40b1ddf0716a64999dd246bc5753062d"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="angeo-41-13-2023-ie00003.svg" width="40pt" height="14pt" src="angeo-41-13-2023-ie00003.png"/></svg:svg></span></span> events at adjacent stations typically occurred simultaneously, the most intense internal (and total) <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M5" display="inline" overflow="scroll" dspmath="mathml"><mrow><mo>|</mo><mi mathvariant="normal">d</mi><mi mathvariant="bold-italic">H</mi><mo>/</mo><mi mathvariant="normal">d</mi><mi>t</mi><mo>|</mo></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="40pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="51a928c613e35e79258f9fbbd657cc8a"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="angeo-41-13-2023-ie00004.svg" width="40pt" height="14pt" src="angeo-41-13-2023-ie00004.png"/></svg:svg></span></span> events were more scattered in time, most likely due to the complexity of induction in the conducting ground. …”
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Global impact of the COVID-19 lockdown on surface concentration and health risk of atmospheric benzene by C. Ling, L. Cui, R. Li, R. Li

“…The detrended change (<span class="inline-formula"><i>P</i>^∗</span>) of the deweathered benzene level (change ratio in 2020 <span class="inline-formula">−</span> change ratio in 2019) followed the order of India (<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M11" display="inline" overflow="scroll" dspmath="mathml"><mrow><msup><mi>P</mi><mo>*</mo></msup><mo>=</mo><mo>-</mo><mn mathvariant="normal">16.2</mn></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="55pt" height="11pt" class="svg-formula" dspmath="mathimg" md5hash="852b46592b1dfc654f40713391ad0a3e"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="acp-23-3311-2023-ie00001.svg" width="55pt" height="11pt" src="acp-23-3311-2023-ie00001.png"/></svg:svg></span></span> %) <span class="inline-formula">&gt;</span> Europe (<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M13" display="inline" overflow="scroll" dspmath="mathml"><mrow><msup><mi>P</mi><mo>∗</mo></msup><mo>=</mo><mo>-</mo><mn mathvariant="normal">13.9</mn></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="55pt" height="11pt" class="svg-formula" dspmath="mathimg" md5hash="712abd5f6894974ee3da4a2af6e00f96"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="acp-23-3311-2023-ie00002.svg" width="55pt" height="11pt" src="acp-23-3311-2023-ie00002.png"/></svg:svg></span></span> %) <span class="inline-formula">&gt;</span> China (<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M15" display="inline" overflow="scroll" dspmath="mathml"><mrow><msup><mi>P</mi><mo>∗</mo></msup><mo>=</mo><mo>-</mo><mn mathvariant="normal">13.3</mn></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="55pt" height="11pt" class="svg-formula" dspmath="mathimg" md5hash="baa35aa5281d9a0ef24f77a794a21914"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="acp-23-3311-2023-ie00003.svg" width="55pt" height="11pt" src="acp-23-3311-2023-ie00003.png"/></svg:svg></span></span> %) <span class="inline-formula">&gt;</span> the United States (<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M17" display="inline" overflow="scroll" dspmath="mathml"><mrow><msup><mi>P</mi><mo>∗</mo></msup><mo>=</mo><mo>-</mo><mn mathvariant="normal">6.00</mn></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="55pt" height="11pt" class="svg-formula" dspmath="mathimg" md5hash="3c55c747468e9828db95e0548fd42fb3"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="acp-23-3311-2023-ie00004.svg" width="55pt" height="11pt" src="acp-23-3311-2023-ie00004.png"/></svg:svg></span></span> %). …”
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Evaluating the Digestibility of Ammonia Fermented (Amofer) Corn Cob Using Different Levels of M21 Decomposer and Urea (In Vitro Study) by Restuti Fitria, Siti Rahmawati Zulaikhah, Novita Hindratiningrum

“…The treatments in this study were the addition of MD and U at different levels. namely R0 = Corn cob without amofer/control; R1 = Amofer Corn cob plus 0.04% MD+3% U; R2 = Amofer Corn cob plus 0.06% MD+3% U; R3 = Amofer Corn cob plus 0.04% MD+5% U; and R4 = Amofer Corn cob plus 0.06% MD+5% U. …”
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SIMULASI KUNCI ELEKTRONIK DENGAN ENKRIPSI MELALUI BLUETOOTH PADA PONSEL by Indri Neforawati, Hoga Saragih

“…Phones that use must support the Java MIDP 2.0 and JSR-82. Keywords: Hashing MD5, Enkripsi RC4, NetBeans IDE 4.1, mysql-connector-java-3.0.9…”
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Network meta-analysis of curative efficacy of different acupuncture methods on obesity combined with insulin resistance by Jiankun Chen, Yingming Gu, Lihong Yin, Minyi He, Na Liu, Yue Lu, Changcai Xie, Jiqiang Li, Yu Chen

“…The results of the network meta-analysis showed that, compared with the control group, three kinds of acupuncture methods (electropuncture, acupoint catgut embedding, and acupuncture point patch) had significant efficacy in reducing FBG [electropuncture (MD = -0.44, 95% CI: -0.83, -0.05) and acupoint catgut embedding (MD = -0.36, 95% CI: -0.51, -0.21)], FINS [electropuncture (MD = -6.17, 95% CI: -9.69, -2.65), acupoint catgut embedding (MD = -5.87, 95% CI: -6.92, -4.82), and acupuncture point patch (MD = -5.86, 95% CI: -11.40, -0.32)], HOMA-IR [electropuncture (MD = -1.59, 95% CI: -2.73, -0.45) and acupoint catgut embedding (MD =-0.91, 95% CI: -1.07, -0.75)], BMI [electropuncture (MD = -1.68, 95% CI: -2.70, -0.66), acupoint catgut embedding (MD = -3.39, 95% CI: -4.38, -2.40), and acupuncture point patch [MD = -2.90, 95%CI: -4.93, -0.87)], and waistline [electropuncture (MD = -5.49, 95% CI: -8.56, -2.42) and acupoint catgut embedding (MD = -4.91, 95% CI: -7.51, -2.31)] in obese patients with insulin resistance, suggesting that their efficacy was better than that of the western medicine group in some of the outcome indicators. …”
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Outcomes of reverse shoulder arthroplasty in patients with previous rotator cuff repair: a systematic review and meta-analysis by Ryan P. Tantone, MD, Samer Al-Humadi, MD, Taylor VanHelmond, BS, Matthew Kim, BA, David E. Komatsu, PhD, Edward D. Wang, MD

“…Average postoperative Constant Score was 62.97 in the RCR group and 66.63 in the group without prior RCR (MD = −5.02, P ≤ .0001, I2 ≤ 0.001). Average postoperative University of California at Los Angeles Shoulder Scale score was 28.27 in the RCR group and 29.13 in the group without prior RCR (MD = −1.75, P ≤ .001, I2 ≤ 0.001). …”
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Mckelveyite group minerals – Part 4: Alicewilsonite-(YLa), Na₂Sr₂YLa(CO₃)₆&thinsp; ⋅ &thinsp;3H₂O, a new lanthanum-dominant s... by I. Lykova, R. Rowe, G. Poirier, H. Friis, K. Helwig

“…The strongest reflections of the powder X-ray diffraction pattern [<span class="inline-formula"><i>d</i></span>,Å(<span class="inline-formula"><i>I</i></span>)(hkl)] are 6.03(43)(001), 4.355(100)(1<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M79" display="inline" overflow="scroll" dspmath="mathml"><mover accent="true"><mn mathvariant="normal">1</mn><mo mathvariant="normal">‾</mo></mover></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="8pt" height="13pt" class="svg-formula" dspmath="mathimg" md5hash="58b89df6a568f22bd126fa17cec2e421"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="ejm-36-301-2024-ie00001.svg" width="8pt" height="13pt" src="ejm-36-301-2024-ie00001.png"/></svg:svg></span></span>0, <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M80" display="inline" overflow="scroll" dspmath="mathml"><mrow><mover accent="true"><mn mathvariant="normal">2</mn><mo mathvariant="normal">‾</mo></mover><mover accent="true"><mn mathvariant="normal">1</mn><mo mathvariant="normal">‾</mo></mover></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="14pt" height="13pt" class="svg-formula" dspmath="mathimg" md5hash="dac27974c69484527cbc2bfef3831989"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="ejm-36-301-2024-ie00002.svg" width="14pt" height="13pt" src="ejm-36-301-2024-ie00002.png"/></svg:svg></span></span>1, 120), 4.020(30)(<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M81" display="inline" overflow="scroll" dspmath="mathml"><mover accent="true"><mn mathvariant="normal">1</mn><mo mathvariant="normal">‾</mo></mover></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="8pt" height="13pt" class="svg-formula" dspmath="mathimg" md5hash="d15d55faba11fbb2897545ff3996eeb3"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="ejm-36-301-2024-ie00003.svg" width="8pt" height="13pt" src="ejm-36-301-2024-ie00003.png"/></svg:svg></span></span>11, 210, <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M82" display="inline" overflow="scroll" dspmath="mathml"><mrow><mover accent="true"><mn mathvariant="normal">1</mn><mo mathvariant="normal">‾</mo></mover><mover accent="true"><mn mathvariant="normal">2</mn><mo mathvariant="normal">‾</mo></mover></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="14pt" height="13pt" class="svg-formula" dspmath="mathimg" md5hash="0fef6d37cc7bc75076f80ec64be63d90"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="ejm-36-301-2024-ie00004.svg" width="14pt" height="13pt" src="ejm-36-301-2024-ie00004.png"/></svg:svg></span></span>1), 3.188(29)(<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M83" display="inline" overflow="scroll" dspmath="mathml"><mrow><mspace width="0.125em" linebreak="nobreak"/><mover accent="true"><mn mathvariant="normal">2</mn><mo mathvariant="normal">‾</mo></mover><mover accent="true"><mn mathvariant="normal">1</mn><mo mathvariant="normal">‾</mo></mover></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="14pt" height="13pt" class="svg-formula" dspmath="mathimg" md5hash="6bd1d55d919bea431e51f1f31693b08e"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="ejm-36-301-2024-ie00005.svg" width="14pt" height="13pt" src="ejm-36-301-2024-ie00005.png"/></svg:svg></span></span>2, 1<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M84" display="inline" overflow="scroll" dspmath="mathml"><mover accent="true"><mn mathvariant="normal">1</mn><mo mathvariant="normal">‾</mo></mover></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="8pt" height="13pt" class="svg-formula" dspmath="mathimg" md5hash="7c5dbfb675e56fab2aad9c252ef1545f"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="ejm-36-301-2024-ie00006.svg" width="8pt" height="13pt" src="ejm-36-301-2024-ie00006.png"/></svg:svg></span></span>1, 121), 2.819(96)(002, <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M85" display="inline" overflow="scroll" dspmath="mathml"><mover accent="true"><mn mathvariant="normal">1</mn><mo mathvariant="normal">‾</mo></mover></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="8pt" height="13pt" class="svg-formula" dspmath="mathimg" md5hash="93134270f7cadb8b0aec402ea46c3d8f"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="ejm-36-301-2024-ie00007.svg" width="8pt" height="13pt" src="ejm-36-301-2024-ie00007.png"/></svg:svg></span></span>12, 211, <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M86" display="inline" overflow="scroll" dspmath="mathml"><mrow><mover accent="true"><mn mathvariant="normal">1</mn><mo mathvariant="normal">‾</mo></mover><mover accent="true"><mn mathvariant="normal">2</mn><mo mathvariant="normal">‾</mo></mover></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="14pt" height="13pt" class="svg-formula" dspmath="mathimg" md5hash="12713b639de16434216e93ad67c3f7a0"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="ejm-36-301-2024-ie00008.svg" width="14pt" height="13pt" src="ejm-36-301-2024-ie00008.png"/></svg:svg></span></span>2), 2.592(40)(<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M87" display="inline" overflow="scroll" dspmath="mathml"><mover accent="true"><mn mathvariant="normal">3</mn><mo mathvariant="normal">‾</mo></mover></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="8pt" height="13pt" class="svg-formula" dspmath="mathimg" md5hash="9fa9e8dba581cad1e86c88af822ec50f"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="ejm-36-301-2024-ie00009.svg" width="8pt" height="13pt" src="ejm-36-301-2024-ie00009.png"/></svg:svg></span></span>01, 030, <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M88" display="inline" overflow="scroll" dspmath="mathml"><mrow><mover accent="true"><mn mathvariant="normal">3</mn><mo mathvariant="normal">‾</mo></mover><mover accent="true"><mn mathvariant="normal">3</mn><mo mathvariant="normal">‾</mo></mover></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="14pt" height="13pt" class="svg-formula" dspmath="mathimg" md5hash="5c05b18c4d219fbf187e34b20c271026"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="ejm-36-301-2024-ie00010.svg" width="14pt" height="13pt" src="ejm-36-301-2024-ie00010.png"/></svg:svg></span></span>1), 2.228(33)(<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M89" display="inline" overflow="scroll" dspmath="mathml"><mover accent="true"><mn mathvariant="normal">2</mn><mo mathvariant="normal">‾</mo></mover></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="8pt" height="13pt" class="svg-formula" dspmath="mathimg" md5hash="9b9d4b7da08f01ac1b26235632266996"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="ejm-36-301-2024-ie00011.svg" width="8pt" height="13pt" src="ejm-36-301-2024-ie00011.png"/></svg:svg></span></span>21, <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M90" display="inline" overflow="scroll" dspmath="mathml"><mrow><mover accent="true"><mn mathvariant="normal">4</mn><mo mathvariant="normal">‾</mo></mover><mover accent="true"><mn mathvariant="normal">2</mn><mo mathvariant="normal">‾</mo></mover></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="14pt" height="13pt" class="svg-formula" dspmath="mathimg" md5hash="a728b56d26a8df380354fb4e8b7bc12b"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="ejm-36-301-2024-ie00012.svg" width="14pt" height="13pt" src="ejm-36-301-2024-ie00012.png"/></svg:svg></span></span>1, <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M91" display="inline" overflow="scroll" dspmath="mathml"><mrow><mover accent="true"><mn mathvariant="normal">2</mn><mo mathvariant="normal">‾</mo></mover><mover accent="true"><mn mathvariant="normal">4</mn><mo mathvariant="normal">‾</mo></mover></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="14pt" height="13pt" class="svg-formula" dspmath="mathimg" md5hash="437febe734386a4124c8e0b63df27bf7"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="ejm-36-301-2024-ie00013.svg" width="14pt" height="13pt" src="ejm-36-301-2024-ie00013.png"/></svg:svg></span></span>1). 2.011(36)(<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M92" display="inline" overflow="scroll" dspmath="mathml"><mover accent="true"><mn mathvariant="normal">2</mn><mo mathvariant="normal">‾</mo></mover></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="8pt" height="13pt" class="svg-formula" dspmath="mathimg" md5hash="4c640149faf94bed07b44fa2ccacc6f7"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="ejm-36-301-2024-ie00014.svg" width="8pt" height="13pt" src="ejm-36-301-2024-ie00014.png"/></svg:svg></span></span>22, 003, 420, <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M93" display="inline" overflow="scroll" dspmath="mathml"><mrow><mover accent="true"><mn mathvariant="normal">2</mn><mo mathvariant="normal">‾</mo></mover><mover accent="true"><mn mathvariant="normal">4</mn><mo mathvariant="normal">‾</mo></mover></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="14pt" height="13pt" class="svg-formula" dspmath="mathimg" md5hash="ad2beb7dab081b5772b140f06afa4615"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="ejm-36-301-2024-ie00015.svg" width="14pt" height="13pt" src="ejm-36-301-2024-ie00015.png"/></svg:svg></span></span>2), 1.9671(32)(<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M94" display="inline" overflow="scroll" dspmath="mathml"><mover accent="true"><mn mathvariant="normal">3</mn><mo mathvariant="normal">‾</mo></mover></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="8pt" height="13pt" class="svg-formula" dspmath="mathimg" md5hash="5da2cd8f0b343e467ab7093d639dc1d0"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="ejm-36-301-2024-ie00016.svg" width="8pt" height="13pt" src="ejm-36-301-2024-ie00016.png"/></svg:svg></span></span>03, 301, 0<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M95" display="inline" overflow="scroll" dspmath="mathml"><mover accent="true"><mn mathvariant="normal">3</mn><mo mathvariant="normal">‾</mo></mover></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="8pt" height="13pt" class="svg-formula" dspmath="mathimg" md5hash="c6472df561403b9adee12ede6c55cbc1"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="ejm-36-301-2024-ie00017.svg" width="8pt" height="13pt" src="ejm-36-301-2024-ie00017.png"/></svg:svg></span></span>2, 032, <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M96" display="inline" overflow="scroll" dspmath="mathml"><mrow><mover accent="true"><mn mathvariant="normal">3</mn><mo mathvariant="normal">‾</mo></mover><mover accent="true"><mn mathvariant="normal">3</mn><mo mathvariant="normal">‾</mo></mover></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="14pt" height="13pt" class="svg-formula" dspmath="mathimg" md5hash="0302da968ec247513629afa45878d94a"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="ejm-36-301-2024-ie00018.svg" width="14pt" height="13pt" src="ejm-36-301-2024-ie00018.png"/></svg:svg></span></span>3, 331). …”
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Towards a conceptualization of the hydrological processes behind changes of young water fraction with elevation: a focus on mountainous alpine catchments by A. Gentile, D. Canone, N. Ceperley, N. Ceperley, D. Gisolo, M. Previati, G. Zuecco, G. Zuecco, B. Schaefli, B. Schaefli, S. Ferraris

“…<p>The young water fraction (<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M1" display="inline" overflow="scroll" dspmath="mathml"><mrow><msubsup><mi>F</mi><mi mathvariant="normal">yw</mi><mo>*</mo></msubsup></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="18pt" height="15pt" class="svg-formula" dspmath="mathimg" md5hash="1cb5ee18b0e8376968be745628e33e91"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="hess-27-2301-2023-ie00001.svg" width="18pt" height="15pt" src="hess-27-2301-2023-ie00001.png"/></svg:svg></span></span>), defined as the fraction of catchment outflow with transit times of less than 2–3 months, is increasingly used in hydrological studies that exploit the potential of isotope tracers. …”
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On the treatment of discordant detrital zircon U–Pb data by P. Vermeesch

“…Constructing (detrital) U–Pb age spectra is straightforward for concordant <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M1" display="inline" overflow="scroll" dspmath="mathml"><mrow class="chem"><msup><mi/><mn mathvariant="normal">206</mn></msup><mi mathvariant="normal">Pb</mi><msup><mo>/</mo><mn mathvariant="normal">238</mn></msup><mi mathvariant="normal">U</mi></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="57pt" height="15pt" class="svg-formula" dspmath="mathimg" md5hash="31944126169e2299ed307f6a1515a652"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="gchron-3-247-2021-ie00001.svg" width="57pt" height="15pt" src="gchron-3-247-2021-ie00001.png"/></svg:svg></span></span> and <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M2" display="inline" overflow="scroll" dspmath="mathml"><mrow class="chem"><msup><mi/><mn mathvariant="normal">207</mn></msup><mi mathvariant="normal">Pb</mi><msup><mo>/</mo><mn mathvariant="normal">206</mn></msup><mi mathvariant="normal">Pb</mi></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="63pt" height="15pt" class="svg-formula" dspmath="mathimg" md5hash="357cb3087249c98aa6409e1f05c396b9"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="gchron-3-247-2021-ie00002.svg" width="63pt" height="15pt" src="gchron-3-247-2021-ie00002.png"/></svg:svg></span></span> compositions. …”
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Simultaneous formation of sulfate and nitrate via co-uptake of SO₂ and NO₂ by aqueous NaCl droplets: combined effect of nitrate photolysis and chlorine chemis... by R. Zhang, R. Zhang, C. K. Chan, C. K. Chan, C. K. Chan, C. K. Chan

“…To parameterize the role of nitrate photolysis and chloride photolysis in forming sulfate, the SO<span class="inline-formula">₂</span> uptake coefficient, <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M22" display="inline" overflow="scroll" dspmath="mathml"><mrow><msub><mi mathvariant="italic">γ</mi><mrow class="chem"><msub><mi mathvariant="normal">SO</mi><mn mathvariant="normal">2</mn></msub></mrow></msub></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="23pt" height="12pt" class="svg-formula" dspmath="mathimg" md5hash="7b9410df74d6fda480a64fc8606aaf92"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="acp-23-6113-2023-ie00002.svg" width="23pt" height="12pt" src="acp-23-6113-2023-ie00002.png"/></svg:svg></span></span>, as a function of the nitrate photolysis rate, <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M23" display="inline" overflow="scroll" dspmath="mathml"><mrow><msub><mi>P</mi><mrow class="chem"><msubsup><mi mathvariant="normal">NO</mi><mn mathvariant="normal">3</mn><mo>-</mo></msubsup></mrow></msub></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="25pt" height="16pt" class="svg-formula" dspmath="mathimg" md5hash="da19ac2768e7dcd8b97125e02ffb8017"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="acp-23-6113-2023-ie00003.svg" width="25pt" height="16pt" src="acp-23-6113-2023-ie00003.png"/></svg:svg></span></span> (<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M24" display="inline" overflow="scroll" dspmath="mathml"><mrow><msub><mi>j</mi><mrow class="chem"><msubsup><mi mathvariant="normal">NO</mi><mn mathvariant="normal">3</mn><mo>-</mo></msubsup></mrow></msub></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="23pt" height="16pt" class="svg-formula" dspmath="mathimg" md5hash="a1ec66b903008f20411aa0f52124fb6e"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="acp-23-6113-2023-ie00004.svg" width="23pt" height="16pt" src="acp-23-6113-2023-ie00004.png"/></svg:svg></span></span> <span class="inline-formula">×</span> [NO<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M26" display="inline" overflow="scroll" dspmath="mathml"><mrow><msubsup><mi/><mn mathvariant="normal">3</mn><mo>-</mo></msubsup></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="9pt" height="16pt" class="svg-formula" dspmath="mathimg" md5hash="d96e0e0e6a6172a7d34ac185b1d0a8a7"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="acp-23-6113-2023-ie00005.svg" width="9pt" height="16pt" src="acp-23-6113-2023-ie00005.png"/></svg:svg></span></span>]), and chloride photolysis rate, <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M27" display="inline" overflow="scroll" dspmath="mathml"><mrow><msub><mi>P</mi><mrow class="chem"><msup><mi mathvariant="normal">Cl</mi><mo>-</mo></msup></mrow></msub></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="21pt" height="12pt" class="svg-formula" dspmath="mathimg" md5hash="c20a22d03150bc6a02a165a42d80bf4f"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="acp-23-6113-2023-ie00006.svg" width="21pt" height="12pt" src="acp-23-6113-2023-ie00006.png"/></svg:svg></span></span> (<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M28" display="inline" overflow="scroll" dspmath="mathml"><mrow><msub><mi>j</mi><mrow class="chem"><msup><mi mathvariant="normal">Cl</mi><mo>-</mo></msup></mrow></msub></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="19pt" height="12pt" class="svg-formula" dspmath="mathimg" md5hash="5a5e5821e30a4aa083481a712d7b2f61"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="acp-23-6113-2023-ie00007.svg" width="19pt" height="12pt" src="acp-23-6113-2023-ie00007.png"/></svg:svg></span></span> <span class="inline-formula">×</span> [Cl<span class="inline-formula">⁻</span>]), was derived as <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M31" display="inline" overflow="scroll" dspmath="mathml"><mrow><msub><mi mathvariant="italic">γ</mi><mrow class="chem"><msub><mi mathvariant="normal">SO</mi><mn mathvariant="normal">2</mn></msub></mrow></msub></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="23pt" height="12pt" class="svg-formula" dspmath="mathimg" md5hash="80233142351d2e72f6461524fc3ad109"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="acp-23-6113-2023-ie00008.svg" width="23pt" height="12pt" src="acp-23-6113-2023-ie00008.png"/></svg:svg></span></span> <span class="inline-formula">=</span> 0.41 <span class="inline-formula">×</span> <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M34" display="inline" overflow="scroll" dspmath="mathml"><mrow><msub><mi>P</mi><mrow class="chem"><msubsup><mi mathvariant="normal">NO</mi><mn mathvariant="normal">3</mn><mo>-</mo></msubsup></mrow></msub></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="25pt" height="16pt" class="svg-formula" dspmath="mathimg" md5hash="b0783186d815e9fba508cdfddc2f7861"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="acp-23-6113-2023-ie00009.svg" width="25pt" height="16pt" src="acp-23-6113-2023-ie00009.png"/></svg:svg></span></span> <span class="inline-formula">+</span> 0.34 <span class="inline-formula">×</span> <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M37" display="inline" overflow="scroll" dspmath="mathml"><mrow><msub><mi>P</mi><mrow class="chem"><msup><mi mathvariant="normal">Cl</mi><mo>-</mo></msup></mrow></msub></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="21pt" height="12pt" class="svg-formula" dspmath="mathimg" md5hash="6c8feedebb5852880e99969496449ecd"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="acp-23-6113-2023-ie00010.svg" width="21pt" height="12pt" src="acp-23-6113-2023-ie00010.png"/></svg:svg></span></span>. …”
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Source apportionment and evolution of N-containing aerosols at a rural cloud forest in Taiwan by isotope analysis by T.-Y. Chen, C.-L. Chen, Y.-C. Chen, C. C.-K. Chou, H. Ren, H.-M. Hung

“…The higher <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M7" display="inline" overflow="scroll" dspmath="mathml"><mrow class="chem"><msup><msub><mi mathvariant="normal">NH</mi><mn mathvariant="normal">4</mn></msub><mo>+</mo></msup></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="29pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="c758f8e5a6278666d33ae83e108e9e6f"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="acp-22-13001-2022-ie00003.svg" width="29pt" height="14pt" src="acp-22-13001-2022-ie00003.png"/></svg:svg></span></span> concentration in fine particles under foggy conditions corresponds to submicron-sized <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M8" display="inline" overflow="scroll" dspmath="mathml"><mrow class="chem"><msup><msub><mi mathvariant="normal">NO</mi><mn mathvariant="normal">3</mn></msub><mo>-</mo></msup></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="30pt" height="15pt" class="svg-formula" dspmath="mathimg" md5hash="42687a47ce11667afdef3248d4b878b5"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="acp-22-13001-2022-ie00004.svg" width="30pt" height="15pt" src="acp-22-13001-2022-ie00004.png"/></svg:svg></span></span> formation via aqueous-phase dissolution with <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M9" display="inline" overflow="scroll" dspmath="mathml"><mrow class="chem"><msup><msub><mi mathvariant="normal">NH</mi><mn mathvariant="normal">4</mn></msub><mo>+</mo></msup></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="29pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="13875b38dd02034385acbae35b139293"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="acp-22-13001-2022-ie00005.svg" width="29pt" height="14pt" src="acp-22-13001-2022-ie00005.png"/></svg:svg></span></span> neutralization. …”
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Charcoal morphologies and morphometrics of a Eurasian grass-dominated system for robust interpretation of past fuel and fire type by A. Feurdean, A. Feurdean, R. S. Vachula, D. Hanganu, D. Hanganu, A. Stobbe, M. Gumnior

“…Morphometric analyses revealed that graminoid charcoal particles were more elongated (length-to-width ratio <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M1" display="inline" overflow="scroll" dspmath="mathml"><mrow><mi>L</mi><mo>/</mo><mi>W</mi><mo>=</mo><mn mathvariant="normal">4</mn></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="45pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="29fe76cb39b2a1899c0c65715a24f714"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="bg-20-5069-2023-ie00001.svg" width="45pt" height="14pt" src="bg-20-5069-2023-ie00001.png"/></svg:svg></span></span>) and narrower (width-to-length ratio <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M2" display="inline" overflow="scroll" dspmath="mathml"><mrow><mi>W</mi><mo>/</mo><mi>L</mi><mo>=</mo><mn mathvariant="normal">0.38</mn></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="58pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="10fef18f1ef48085a16ac96a9614798c"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="bg-20-5069-2023-ie00002.svg" width="58pt" height="14pt" src="bg-20-5069-2023-ie00002.png"/></svg:svg></span></span>) than forbs (<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M3" display="inline" overflow="scroll" dspmath="mathml"><mrow><mi>L</mi><mo>/</mo><mi>W</mi><mo>=</mo><mn mathvariant="normal">3.1</mn></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="54pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="92b7c3c5bce26f6d3716a15e8fd96d51"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="bg-20-5069-2023-ie00003.svg" width="54pt" height="14pt" src="bg-20-5069-2023-ie00003.png"/></svg:svg></span></span> and <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M4" display="inline" overflow="scroll" dspmath="mathml"><mrow><mi>W</mi><mo>/</mo><mi>L</mi><mo>=</mo><mn mathvariant="normal">0.42</mn></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="58pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="01c783080b11371d1291698c5a743e08"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="bg-20-5069-2023-ie00004.svg" width="58pt" height="14pt" src="bg-20-5069-2023-ie00004.png"/></svg:svg></span></span>, respectively), in agreement with a global compilation for graminoids (<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M5" display="inline" overflow="scroll" dspmath="mathml"><mrow><mi>L</mi><mo>/</mo><mi>W</mi><mo>=</mo><mn mathvariant="normal">4.3</mn></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="54pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="cf6cd745c7d94ae8e9d1a8f91e71f2a4"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="bg-20-5069-2023-ie00005.svg" width="54pt" height="14pt" src="bg-20-5069-2023-ie00005.png"/></svg:svg></span></span> for grass 5.4 grass and wetland graminoids) and forbs (<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M6" display="inline" overflow="scroll" dspmath="mathml"><mrow><mi>L</mi><mo>/</mo><mi>W</mi><mo>=</mo><mn mathvariant="normal">2.9</mn></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="54pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="5b307ff3121851903d2b4d9840f8bd7c"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="bg-20-5069-2023-ie00006.svg" width="54pt" height="14pt" src="bg-20-5069-2023-ie00006.png"/></svg:svg></span></span>). …”
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A regolith lead isoscape of Australia by C. U. Desem, P. de Caritat, J. Woodhead, R. Maas, G. Carr

“…<p>We present the first national-scale lead (Pb) isotope maps of Australia based on surface regolith for five isotope ratios, <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M1" display="inline" overflow="scroll" dspmath="mathml"><mrow class="chem"><msup><mi/><mn mathvariant="normal">206</mn></msup><mi mathvariant="normal">Pb</mi><msup><mo>/</mo><mn mathvariant="normal">204</mn></msup><mi mathvariant="normal">Pb</mi></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="63pt" height="15pt" class="svg-formula" dspmath="mathimg" md5hash="e2b4c152d04a98c71ee6378c00fe9403"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="essd-16-1383-2024-ie00001.svg" width="63pt" height="15pt" src="essd-16-1383-2024-ie00001.png"/></svg:svg></span></span>, <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M2" display="inline" overflow="scroll" dspmath="mathml"><mrow class="chem"><msup><mi/><mn mathvariant="normal">207</mn></msup><mi mathvariant="normal">Pb</mi><msup><mo>/</mo><mn mathvariant="normal">204</mn></msup><mi mathvariant="normal">Pb</mi></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="63pt" height="15pt" class="svg-formula" dspmath="mathimg" md5hash="00c58db6d3703defb753bdb5f603e392"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="essd-16-1383-2024-ie00002.svg" width="63pt" height="15pt" src="essd-16-1383-2024-ie00002.png"/></svg:svg></span></span>, <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M3" display="inline" overflow="scroll" dspmath="mathml"><mrow class="chem"><msup><mi/><mn mathvariant="normal">208</mn></msup><mi mathvariant="normal">Pb</mi><msup><mo>/</mo><mn mathvariant="normal">204</mn></msup><mi mathvariant="normal">Pb</mi></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="63pt" height="15pt" class="svg-formula" dspmath="mathimg" md5hash="66f6e34b561fbf86cfd77d9762478a32"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="essd-16-1383-2024-ie00003.svg" width="63pt" height="15pt" src="essd-16-1383-2024-ie00003.png"/></svg:svg></span></span>, <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M4" display="inline" overflow="scroll" dspmath="mathml"><mrow class="chem"><msup><mi/><mn mathvariant="normal">207</mn></msup><mi mathvariant="normal">Pb</mi><msup><mo>/</mo><mn mathvariant="normal">206</mn></msup><mi mathvariant="normal">Pb</mi></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="63pt" height="15pt" class="svg-formula" dspmath="mathimg" md5hash="ce5d752788a0b117b55e8c8cb1d33bf0"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="essd-16-1383-2024-ie00004.svg" width="63pt" height="15pt" src="essd-16-1383-2024-ie00004.png"/></svg:svg></span></span>, and <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M5" display="inline" overflow="scroll" dspmath="mathml"><mrow class="chem"><msup><mi/><mn mathvariant="normal">208</mn></msup><mi mathvariant="normal">Pb</mi><msup><mo>/</mo><mn mathvariant="normal">206</mn></msup><mi mathvariant="normal">Pb</mi></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="63pt" height="15pt" class="svg-formula" dspmath="mathimg" md5hash="fa062e689928bc0d0a62d3c3ecf8be6f"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="essd-16-1383-2024-ie00005.svg" width="63pt" height="15pt" src="essd-16-1383-2024-ie00005.png"/></svg:svg></span></span>, determined by single-collector sector field inductively coupled plasma mass spectrometry after an ammonium acetate leach followed by aqua regia digestion. …”
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Desorption lifetimes and activation energies influencing gas–surface interactions and multiphase chemical kinetics by D. A. Knopf, D. A. Knopf, M. Ammann, T. Berkemeier, U. Pöschl, M. Shiraiwa

“…The desorption energy (<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M1" display="inline" overflow="scroll" dspmath="mathml"><mrow><msubsup><mi>E</mi><mi mathvariant="normal">des</mi><mn mathvariant="normal">0</mn></msubsup></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="22pt" height="17pt" class="svg-formula" dspmath="mathimg" md5hash="967d81a968069b468196769f6a46c796"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="acp-24-3445-2024-ie00001.svg" width="22pt" height="17pt" src="acp-24-3445-2024-ie00001.png"/></svg:svg></span></span>), which depends on the intermolecular forces between adsorbate and substrate, determines the residence time of chemical species at interfaces. …”
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Dinoflagellate cyst and pollen assemblages as tracers for marine productivity and river input in the northern Gulf of Mexico by Y. W. Yedema, T. Donders, F. Peterse, F. Sangiorgi

“…Additionally, the RDA confirmed that the <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M5" display="inline" overflow="scroll" dspmath="mathml"><mrow><mi>H</mi><mo>/</mo><mi>A</mi></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="22pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="e612397d9f3df24db4dde93b9c975102"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="jm-42-257-2023-ie00005.svg" width="22pt" height="14pt" src="jm-42-257-2023-ie00005.png"/></svg:svg></span></span> ratio indeed seems to track primary productivity, while the <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M6" display="inline" overflow="scroll" dspmath="mathml"><mrow><mi>P</mi><mo>/</mo><mi>B</mi></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="23pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="67f79a7edf7ce2c0ba2f7c7208180fc0"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="jm-42-257-2023-ie00006.svg" width="23pt" height="14pt" src="jm-42-257-2023-ie00006.png"/></svg:svg></span></span> ratio results in a robust indicator for distance to the coast, and the <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M7" display="inline" overflow="scroll" dspmath="mathml"><mrow><mi>P</mi><mo>/</mo><mi>D</mi></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="23pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="141f3a48f865d92c4ef19785b57e6370"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="jm-42-257-2023-ie00007.svg" width="23pt" height="14pt" src="jm-42-257-2023-ie00007.png"/></svg:svg></span></span> ratio better reflects river input. …”
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Nitrous oxide (N₂O) synthesis by the freshwater cyanobacterium <i>Microcystis aeruginosa</i> by F. Fabisik, B. Guieysse, J. Procter, M. Plouviez

“…N<span class="inline-formula">₂</span>O production was also positively correlated to the initial NO<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M12" display="inline" overflow="scroll" dspmath="mathml"><mrow><msubsup><mi/><mn mathvariant="normal">2</mn><mo>-</mo></msubsup></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="9pt" height="16pt" class="svg-formula" dspmath="mathimg" md5hash="71c4f283853e1c63b082e22081694bf1"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="bg-20-687-2023-ie00003.svg" width="9pt" height="16pt" src="bg-20-687-2023-ie00003.png"/></svg:svg></span></span> and <i>M. aeruginosa</i> concentrations but was low to negligible when nitrate (NO<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M13" display="inline" overflow="scroll" dspmath="mathml"><mrow><msubsup><mi/><mn mathvariant="normal">3</mn><mo>-</mo></msubsup></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="9pt" height="16pt" class="svg-formula" dspmath="mathimg" md5hash="a192f22c747584054322d55d69a940ca"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="bg-20-687-2023-ie00004.svg" width="9pt" height="16pt" src="bg-20-687-2023-ie00004.png"/></svg:svg></span></span>) and ammonium (NH<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M14" display="inline" overflow="scroll" dspmath="mathml"><mrow><msubsup><mi/><mn mathvariant="normal">4</mn><mo>+</mo></msubsup></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="8pt" height="15pt" class="svg-formula" dspmath="mathimg" md5hash="d0f05de3ef9fdb7d2948354df3a21cd8"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="bg-20-687-2023-ie00005.svg" width="8pt" height="15pt" src="bg-20-687-2023-ie00005.png"/></svg:svg></span></span>) were supplied as the sole exogenous N source instead of NO<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M15" display="inline" overflow="scroll" dspmath="mathml"><mrow><msubsup><mi/><mn mathvariant="normal">2</mn><mo>-</mo></msubsup></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="9pt" height="16pt" class="svg-formula" dspmath="mathimg" md5hash="605864571c3dcb0b6e3cb32dc4ee1961"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="bg-20-687-2023-ie00006.svg" width="9pt" height="16pt" src="bg-20-687-2023-ie00006.png"/></svg:svg></span></span>. …”
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Short communication: Inverse isochron regression for Re–Os, K–Ca and other chronometers by Y. Li, P. Vermeesch

“…<p>Conventional Re–Os isochrons are based on mass spectrometric estimates of <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M1" display="inline" overflow="scroll" dspmath="mathml"><mrow class="chem"><msup><mi/><mn mathvariant="normal">187</mn></msup><mi mathvariant="normal">Re</mi><msup><mo>/</mo><mn mathvariant="normal">188</mn></msup><mi mathvariant="normal">Os</mi></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="64pt" height="15pt" class="svg-formula" dspmath="mathimg" md5hash="ddb9b773837d7735adead78fc4c3577a"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="gchron-3-415-2021-ie00001.svg" width="64pt" height="15pt" src="gchron-3-415-2021-ie00001.png"/></svg:svg></span></span> and <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M2" display="inline" overflow="scroll" dspmath="mathml"><mrow class="chem"><msup><mi/><mn mathvariant="normal">187</mn></msup><mi mathvariant="normal">Os</mi><msup><mo>/</mo><mn mathvariant="normal">188</mn></msup><mi mathvariant="normal">Os</mi></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="64pt" height="15pt" class="svg-formula" dspmath="mathimg" md5hash="421e33d94156b20892e5c16c5a214d7a"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="gchron-3-415-2021-ie00002.svg" width="64pt" height="15pt" src="gchron-3-415-2021-ie00002.png"/></svg:svg></span></span>, which often exhibit strong error correlations that may obscure potentially important geological complexity. …”
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Accurately calibrated X-ray fluorescence core scanning (XRF-CS) record of Ti&thinsp;∕&thinsp;Al reveals Early Pleistocene aridity and humidity variability over North Africa and its... by R. Hennekam, K. M. Grant, E. J. Rohling, E. J. Rohling, R. Tjallingii, D. Heslop, A. P. Roberts, L. J. Lourens, G.-J. Reichart, G.-J. Reichart

“…<p>In eastern Mediterranean sediments, the titanium-to-aluminum ratio (<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M3" display="inline" overflow="scroll" dspmath="mathml"><mrow class="chem"><mi mathvariant="normal">Ti</mi><mo>/</mo><mi mathvariant="normal">Al</mi></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="27pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="64481113532f6f6aaedbbc4986bb9f3d"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="cp-18-2509-2022-ie00004.svg" width="27pt" height="14pt" src="cp-18-2509-2022-ie00004.png"/></svg:svg></span></span>) captures relative variability in eolian to river-derived material and predominantly integrates climate signals over the Saharan and Sahel regions. …”
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