251 research outputs found

    Increased root oxygen uptake in pea plants responding to non-self neighbors

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    Recent studies have demonstrated that plants alter root growth and decrease competition with roots of the same individual (self); however, the physiological traits accompanying this response are still widely unknown. In this study, we investigated the effect of root identity on gas exchange in the model species pea (Pisum sativum L.). Split-root plants were planted so that each pot contained either two roots of the same plant (self) or of two different plants (non-self), and the responses of biomass, photosynthesis, and respiration were measured. The photosynthetic rate was not affected by the identity of the root neighbor. We found a reduction of leaf dark respiration by half, accompanied by an increase in nocturnal root respiration by 29 % in plants neighboring with non-self. The activity of the alternative oxidase (AOX) pathway increased when plants responded to non-self neighbors. The increased activity of AOX in plants responding to non-self indicates carbon imbalances in roots, possibly as a consequence of increased root exudation and communication between individuals. If such an effect occurs more widely, it may change the assumptions made for the quantity of respiration as used in carbon budget models

    Observing soil organic carbon spatial and seasonal variability at the Golan Heights using CO2/O2 fluxes measurements in an incubation experiment

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    Soil organic matter (SOM) stores most of the terrestrial carbon, and changes in this storage can have a significant effect on the global carbon cycle. Various approaches have been used to understand the SOM transformations and stability. Here we measured the respiratory CO2 and O2 fluxes, and their ratio (the Apparent Respiratory Quotient - ARQ) in soil incubations at different temperatures, to learn about the short-term processes affecting SOM stability. To study in detail the spatial and temporal variability, we examine soil samples from two sample sets: a regional set, and a local set that was used to study the seasonality and environmental variability within a site. The regional set was taken from 11 sites located in the north and center of the Golan Heights, the samplings took place in two campaigns in October 2020 and in January 2021. In each site, the sample was pooled from 2 sub-samples taken by a trowel from A-horizon at 0-10 cm depth in adjacent locations. The local soil samples set was taken from Mt. Baron, a volcanic cinder cone which is located in the north of Golan Heights. The sampling took place in October 2021, February 2022, and June 2022, which represent the beginning, middle, and end of the rainy season. Each sample was pooled from 2 locations and taken by a trowel from A-horizon at 0-10 cm depth. At each campaign, the soil was sampled at 4 heights along the north and south slopes, under tree canopy, and in open grassland. The incubations were conducted on fresh sieved soil (2mm), wetted with distilled water to different levels. To explore the effect of anaerobic microsites on ARQ we incubated artificial clods (1 cm diameter) with wetted soil from Mt. Baron (The local set). To further test the effects of O2 limitation we conducted an experiment in which we mitigated this limitation by enriching in oxygen the atmosphere of the incubation headspace. All the incubations were carried out at the Hebrew University of Jerusalem

    Observing soil organic carbon spatial and seasonal variability at the Golan Heights using Rock-Eval measurements

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    Soil organic matter (SOM) stores most of the terrestrial carbon, and changes in this storage can have a significant effect on the global carbon cycle. Various approaches have been used to understand the SOM transformations and stability. Here, we estimated the long-term SOM stability, and the effect of decomposition on the stability and composition of the remaining fraction, by Rock-Eval pyrolysis. The sampling took place in Mount Baron, the Golan Heights, in October 2021, February 2022, and June 2022, which represent the beginning, middle, and end of the rainy season. . Each sample was pooled from 2 locations and taken by a trowel from A-horizon at 0-10 cm depth.. At each campaign, the soil was sampled at 4 heights along the north and south slopes, under tree canopy, and in open grassland. In addition, to study the different fractions of organic matter, we analyzed soil separated into particulate organic matter (POM) and mineral-associated organic matter (MAOM). The samples were dried to 55°C and were ground with a mortar and pestle before the Rock-Eval analysis (Rock Eval 6, Vinci Technologies, at Ben Gurion University of the Negev for October samples and Rock Eval 7S, Vinci Technologies, at the Geological Survey of Israel for February and June samples)

    Replication Data for: Do Personality Traits Predict Voter Attitudes When Politics Is Structured Around Conflict? Lessons From Israel

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    The relationship between personality traits and political attitudes has been studied extensively. However, existing accounts largely study personality’s links to liberal-conservative divisions on social and economic issues. We know far less about its attitudinal influences when politics is organized around other issue domains, particularly ethnonational conflicts. Addressing this gap, we examine the relationship between the Big Five personality traits, policy preferences, and political orientation in Israel, where the main ideological cleavage involves the Israeli-Palestinian conflict. Using original survey data, we find that the known relationships with social and economic attitudes operate only partly and more weakly in this context. Unlike these domains, conflict-related preferences in Israel correlate primarily with greater conscientiousness, largely through authoritarian tendencies. General Left-Right orientations mimic this relationship, reflecting conflict-related views rather than social or economic inclinations. These findings expand the scope of current debates about personality and political attitudes and underscore the importance of national ideological contexts for future research

    A high performance transparent resistive switching memory made from ZrO2/AlON bilayer structure

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    In this study, the switching properties of an indium tin oxide (ITO)/zirconium oxide (ZrO2)/ITO single layer device and those of a device with an aluminum oxynitride (AlON) layer were investigated. The devices with highly transparent characteristics were fabricated. Compared with the ITO/ZrO2/ITO single layer device, the ITO/ZrO2/AlON/ITO bilayer device exhibited a larger ON/OFF ratio, higher endurance performance, and superior retention properties by using a simple two-step forming process. These substantial improvements in the resistive switching properties were attributed to the minimized influence of oxygen migration through the ITO top electrode (TE), which can be realized by forming an asymmetrical conductive filament with the weakest part at the ZrO2/AlON interface. Therefore, in the ITO/ZrO2/AlON/ITO bilayer device, the regions where conductive filament formation and rupture occur can be effectively moved from the TE interface to the interior of the device. Published by AIP Publishing.Ministry of Science and Technology, Taiwan [NSC 102-2221-E009-134-MY3]SCI(E)[email protected]

    Oxygen Isotope Signatures of Phosphate in Wildfire Ash

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    Atmospheric aerosol deposition is a significant source of phosphorus (P) in many terrestrial and marine ecosystems worldwide, influencing their biogeochemistry and primary production. Particles emitted from wildfires (hereafter, ash) are the second most important source of atmospheric P after airborne dust. In this study, we aim to identify the signature of ash oxygen isotopes in phosphate. This will enable the use of this signature for the separation of ash from other atmospheric P sources. We measured P concentrations and δ18OP in ash from natural and experimental fires and also from ash heated at different temperatures. The HCl and resin P concentrations (average ± SE) were 3.15 ± 0.35 and 1 ± 0.1 mg g–1, respectively. The HCl and resin δ18OP were 15.5 ± 0.4 and 14.7 ± 0.4‰ (average ± SE), respectively. Based on previous studies, we suggest possible isotope exchange reactions during the combustion process, between oxygen in phosphate and oxygen from other probable sources (i.e., the atmosphere, and CaCO3 and CaO formed in the ash). The unique isotopic signature in the ash, ranging from 11.5 to 19.4‰ in the HCl and resin P fractions, is different from that of other atmospheric P sources such as airborne tree pollen, which has δ18OP values between 19.2‰ and 29.6‰, and Saharan-dust samples collected in Israel, which have δ18OP values ranging from 20.7‰ to 22.6‰. Thus, the δ18OP can be used as a marker for identifying atmospheric P from wildfires and for estimating its importance to the global P cycle

    Product structure extension of the Alon--Seymour--Thomas theorem

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    Alon, Seymour and Thomas [1990] proved that every nn-vertex graph excluding KtK_t as a minor has treewidth less than t3/2nt^{3/2}\sqrt{n}. Illingworth, Scott and Wood [2022] recently refined this result by showing that every such graph is a subgraph of some graph with treewidth t2t-2, where each vertex is blown up by a complete graph of order O(tn)O(\sqrt{tn}). Solving an open problem of Illingworth, Scott and Wood [2022], we prove that the treewidth bound can be reduced to 44 while keeping blowups of order Ot(n)O_t(\sqrt{n}). As an extension of the Lipton--Tarjan theorem, in the case of planar graphs, we show that the treewidth can be further reduced to 22, which is best possible. We generalise this result for K3,tK_{3,t}-minor-free graphs, with blowups of order O(tn)O(t\sqrt{n}). This setting includes graphs embeddable on any fixed surface.Title changed, author added, and results for K3,tK_{3,t}-minor-free graphs added in v2. Referee comments incorporated into v
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