Spatial and temporal heterogeneity of soil respiration in a bare-soil Mediterranean olive grove by S. Aranda-Barranco, S. Aranda-Barranco, P. Serrano-Ortiz, P. Serrano-Ortiz, A. S. Kowalski, A. S. Kowalski, E. P. Sánchez-Cañete, E. P. Sánchez-Cañete

“…<span class="inline-formula"><i>R</i>_{s  Under-Tree}</span> represented 39 % of the <span class="inline-formula"><i>R</i>_s</span> of the olive grove. …”
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A synthesis of <i>Sphagnum</i> litterbag experiments: initial leaching losses bias decomposition rate estimates by H. Teickner, H. Teickner, E. Pebesma, K.-H. Knorr

“…Previous research on vascular plants suggests that decomposition rate (<span class="inline-formula"><i>k</i>₀</span>) estimates from litterbag experiments are biased when initial leaching losses (<span class="inline-formula"><i>l</i>₀</span>) are ignored. …”
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Soybean oil, a linoleic acid source, in lamb diets: metabolic, feeding behavior, and ruminal parameters by V. G. O. Lima, L. O. da Silva, J. E. de Freitas Jr., H. D. R. Alba, V. M. Leite, W. P. Silva, D. D. S. Pina, L. C. Leite, C. S. Rodrigues, S. A. Santos, G. G. P. de Carvalho

“…There was a linear reduction in DM (<span class="inline-formula"><i>P</i></span> <span class="inline-formula">=</span> 0.019) and crude protein (<span class="inline-formula"><i>P</i></span> <span class="inline-formula">=</span> 0.007) intake as well as a linear decrease in non-fibrous carbohydrate intake (<span class="inline-formula"><i>P</i></span> <span class="inline-formula">&lt;</span> 0.001) and digestibility (<span class="inline-formula"><i>P</i></span> <span class="inline-formula">=</span> 0.039) due to increased SO inclusion levels. …”
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Effect of colloidal particle size on physicochemical properties and aggregation behaviors of two alkaline soils by Y. Yan, X. Zhang, C. Xu, C. Xu, J. Liu, F. Hu, F. Hu, Z. Geng, Z. Geng

“…Soil colloidal fractions, from two alkaline soils – Anthrosol and Calcisol – were subdivided into three ranges: <span class="inline-formula"><i>d</i>&lt;2</span> <span class="inline-formula">µ</span>m, <span class="inline-formula"><i>d</i>&lt;1</span> <span class="inline-formula">µ</span>m and <span class="inline-formula"><i>d</i>&lt;100</span> nm. …”
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Dacostaite, K(Mg₂Al)[Mg(H₂O)₆]₂(AsO₄)₂F₆&thinsp; ⋅ &thinsp;2H₂O, a new fluoride–arsenate mi... by C. Biagioni, C. Biagioni, D. Mauro, D. Mauro, J. Sejkora, Z. Dolníček, A. Dini, R. Škoda

“…Dacostaite is monoclinic, with a space group of <span class="inline-formula"><i>C</i></span>2/<span class="inline-formula"><i>m</i></span> and <span class="inline-formula"><i>a</i>=12.474(5)</span>, <span class="inline-formula"><i>b</i>=7.198(3)</span>, <span class="inline-formula"><i>c</i>=13.724(6)</span> Å, <span class="inline-formula"><i>β</i>=99.518(13)</span>°, and <span class="inline-formula"><i>V</i>=1215.3(8)</span> Å<span class="inline-formula">³</span>. …”
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Creep enhancement and sliding in a temperate, hard-bedded alpine glacier by J.-P. Roldán-Blasco, A. Gilbert, L. Piard, F. Gimbert, C. Vincent, O. Gagliardini, A. Togaibekov, A. Togaibekov, A. Walpersdorf, N. Maier

“…<p>Glacier internal deformation is usually described by Glen's flow law using two material parameters: the creep factor (<span class="inline-formula"><i>A</i></span>) and the flow law exponent (<span class="inline-formula"><i>n</i></span>). …”
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A compilation of surface inherent optical properties and phytoplankton pigment concentrations from the Atlantic Meridional Transect by T. M. Jordan, G. Dall'Olmo, G. Tilstone, R. J. W. Brewin, F. Nencioli, R. Airs, C. S. Thomas, L. Schlüter

“…<p>In situ measurements of particulate inherent optical properties (IOPs) – absorption (<span class="inline-formula"><i>a</i>_p(<i>λ</i>)</span>), scattering (<span class="inline-formula"><i>b</i>_p(<i>λ</i>)</span>), and beam attenuation (<span class="inline-formula"><i>c</i>_p(<i>λ</i>)</span>) – are crucial for the development of optical algorithms that retrieve biogeochemical quantities such as chlorophyll <span class="inline-formula"><i>a</i></span>, particulate organic carbon (POC), and total suspended matter (TSM). …”
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Towards quantitative reconstruction of past monsoon precipitation based on tetraether membrane lipids in Chinese loess by J. Guo, J. Guo, M. Ziegler, L. Fuchs, Y. Sun, F. Peterse

“…<p>Variations in the oxygen isotope composition (<span class="inline-formula"><i>δ</i>¹⁸</span>O) of cave speleothems and numerous proxy records from loess–paleosol sequences have revealed past variations in East Asian monsoon (EAM) intensity. …”
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Reconstruction of drought and long-rain chronologies since the 17th century in central Japan using intra-annual tree-ring oxygen isotope ratios and documentary records by H. Iizuka, K. Sho, Z. Li, M. Sano, Y. Kato, T. Nakatsuka

“…<p>Oxygen isotope ratios (<span class="inline-formula"><i>δ</i>¹⁸O</span>) of tree-ring cellulose and historical documentary records are widely used to explore the hydroclimatic conditions of the past. …”
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Insights into the tectonic evolution of the Svecofennian orogeny based on in situ Lu–Hf dating of garnet and apatite from Olkiluoto, southwestern Finland by J. Engström, J. Engström, K. Cutts, S. Glorie, E. Heilimo, E. M. Jolis, R. M. Michallik

“…The pressure–temperature (<span class="inline-formula"><i>P</i></span>–<span class="inline-formula"><i>T</i></span>) path for the rocks indicates a prograde evolution, with peak <span class="inline-formula"><i>P</i></span>–<span class="inline-formula"><i>T</i></span> conditions of 3–5 kbar and approximately 700 °C. …”
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A numerical model for duricrust formation by water table fluctuations by C. Fenske, C. Fenske, J. Braun, J. Braun, F. Guillocheau, C. Robin

“…The model is an extension to an existing regolith formation model, where the position of the water table is used to predict the formation of a hardened layer at a rate set by a characteristic timescale, <span class="inline-formula"><i>τ</i></span>, and over a depth set by the range of fluctuations in the water table, <span class="inline-formula"><i>λ</i></span>. …”
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The benefits and trade-offs of multi-variable calibration of the WaterGAP global hydrological model (WGHM) in the Ganges and Brahmaputra basins by H. M. M. Hasan, P. Döll, P. Döll, S.-M. Hosseini-Moghari, F. Papa, A. Güntner, A. Güntner

“…The trade-offs were particularly pronounced in the Ganges basin, in particular between <span class="inline-formula"><i>Q</i></span> and SWSA, as well as between <span class="inline-formula"><i>Q</i></span> and ET. …”
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Exploring the mechanisms of Devonian oceanic anoxia: impact of ocean dynamics, palaeogeography, and orbital forcing by J. Gérard, L. Sablon, J. J. C. Huygh, A.-C. Da Silva, A. Pohl, C. Vérard, M. Crucifix

“…We quantify the impact of continental configuration, ocean–atmosphere biogeochemistry (global mean oceanic <span class="inline-formula">PO₄</span> concentration and atmospheric <span class="inline-formula"><i>p</i></span><span class="inline-formula">O₂</span>), climatic forcing (<span class="inline-formula"><i>p</i></span><span class="inline-formula">CO₂</span>), and astronomical forcing on background oceanic circulation and oxygenation during the Devonian. …”
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Understanding summertime peroxyacetyl nitrate (PAN) formation and its relation to aerosol pollution: insights from high-resolution measurements and modeling by B. Hu, B. Hu, B. Hu, N. Chen, N. Chen, R. Li, M. Huang, M. Huang, M. Huang, J. Chen, J. Chen, Y. Hong, Y. Hong, L. Xu, L. Xu, X. Fan, X. Fan, M. Li, M. Li, L. Tong, Q. Zheng, Y. Yang

“…The MCM model, with an index of agreement (IOA) value of 0.75, effectively investigates PAN formation, performing better during the clean period (<span class="inline-formula"><i>R</i>²</span>: 0.68; slope <span class="inline-formula"><i>K</i></span>: 0.91) than the haze one (<span class="inline-formula"><i>R</i>²</span>: 0.47; slope <span class="inline-formula"><i>K</i></span>: 0.75). …”
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Effect on OPU/IVEP success of different applications for synchronizing follicular waves prior to superstimulation in holstein heifers by M. F. Çiftçi, Ö. F. Yeşilkaya, S. Ü. Çizmeci, M. Gölbaşı, A. Sarı, D. A. Dinç

“…After these applications, 25 mg of PGF2<span class="inline-formula"><i>α</i></span> was administered intramuscularly on the third and fourth days of treatment. …”
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Computing the time-dependent activity rate using non-declustered and declustered catalogues – a first step towards time-dependent seismic hazard calculations for operational earthq... by D. Montiel-López, S. Molina, S. Molina, J. J. Galiana-Merino, J. J. Galiana-Merino, I. Gómez, I. Gómez, A. Kharazian, J. L. Soler-Llorens, J. A. Huesca-Tortosa, A. Guardiola-Villora, G. Ortuño-Sáez

“…In this work, we propose a methodology that includes the spatially gridded time-dependent <span class="inline-formula"><i>b</i></span> value and activity rate computation using seismic clusters in PSHA calculations. …”
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Imputation of missing land carbon sequestration data in the AR6 Scenarios Database by R. Prütz, R. Prütz, R. Prütz, R. Prütz, S. Fuss, S. Fuss, S. Fuss, J. Rogelj, J. Rogelj, J. Rogelj

“…We find that a <span class="inline-formula"><i>k</i></span>-nearest neighbors regression performs best among the tested regression models and use it to impute and provide two publicly available imputation datasets (<a href="https://doi.org/10.5281/zenodo.13373539">https://doi.org/10.5281/zenodo.13373539</a>, Prütz et al., 2024) on CO<span class="inline-formula">₂</span> removal via land sinks for incomplete global scenarios (<span class="inline-formula"><i>n</i>=404</span>) and incomplete regional R10 scenario variants (<span class="inline-formula"><i>n</i>=2358</span>) of the AR6 Scenarios Database. …”
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Measurement report: Analysis of aerosol optical depth variation at Zhongshan Station in Antarctica by L. Chen, L. Chen, L. Zhang, Y. She, Z. Zeng, Y. Zheng, B. Tian, W. Zhang, Z. Liu, H. Che, M. Ding

“…The temperature and AOD showed an insignificant positive correlation (<span class="inline-formula"><i>R</i></span> <span class="inline-formula">=</span> 0.22, <span class="inline-formula"><i>p</i></span> <span class="inline-formula">=</span> 0.40), and relative humidity exhibited a significant negative correlation with AOD (<span class="inline-formula"><i>R</i></span> <span class="inline-formula">=</span> <span class="inline-formula">−</span>0.59, <span class="inline-formula"><i>p</i></span> <span class="inline-formula">=</span> 0.02). …”
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Aerosol layer height (ALH) retrievals from oxygen absorption bands: intercomparison and validation among different satellite platforms, GEMS, EPIC, and TROPOMI by H. Kim, H. Kim, X. Chen, X. Chen, J. Wang, J. Wang, J. Wang, J. Wang, Z. Lu, Z. Lu, Z. Lu, M. Zhou, G. R. Carmichael, G. R. Carmichael, S. S. Park, J. Kim

“…The GEMS ALH displays minimal bias (0.1 km) but a slightly lower correlation (<span class="inline-formula"><i>R</i></span> <span class="inline-formula">=</span> 0.64). …”
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The Mosquito Repellent Activity of the Active Component of Air Freshener Gel from Java Citronella Oil (Cymbopogon winterianus) by Willy Tirza Eden, Dante Alighiri, Kasmadi Imam Supardi, Edy Cahyono

“…The most significant specific gravity (0.0136) was recorded in formula V, while gel formula I exhibited the highest level of instability at 35°C, with a syneresis value of 77.11% in t=72 h and pH 5.33. …”
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