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Buğday özellikle insanların beslenmesinde büyük rol üstlenmiştir. Yetiştirilmesi son derece zahmetsiz olsada yapılan araştırmalar, iklim değişikliğinden buğdayında olumsuz etkileneceğini ortaya koymuştur. Anadolu’da buğday ekili alanlarda verim ve kaliteyi arttırmak için gübreleme yapılmaktadır. Gübreleme yapılırken uygulanan miktara, uygulama zamanına ve gübre türüne dikkat edilmesi gerekir. Kontrolsüz yapılan gübreleme toprağa ve çevreye zarar vermektedir. Toprağı verimsiz hale getirirken, atmosferede sera gazı salınımına neden olacaktır. Bu durum ise buğday üretiminde ki karbon ayak izinin artmasına neden olacaktır. Yaptığımız bu çalışma da buğday üretimi yapılırken çiftçiler tarafından kullanılan gübrelerin, kullanım miktarına bağlı olarak ürettiği karbon ayak izini hesapladık.

Copyright of Anadolu (1300-0225) is the property of Anadolu Dergisi and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)

Copyright of Anadolu University Journal of the Faculty of Economics & Administrative Sciences is the property of Anadolu University Journal of the Faculty of Economics & Administrative Sciences and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)

Copyright of Düzce University Journal of Forestry / Düzce Üniversitesi Orman Fakültesi Ormancılık Dergisi is the property of Duzce University and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)

This study was carried out in order to reveal the amount of litterfall according to the development stages in the oriental beech forests in the Marmara Region and the carbon stocks input into forest floor in this way. The research was conducted in a total of 18 sample plots, which differ in terms of aspect, elevation, slope, slope position and stand development stages namely the b (dbh=8.0-19,9 cm), c (dbh=20.0-35.9 cm) and d stages (dbh=36.0-51.9 cm). Five litter traps (50×50 cm) were set up each sample plot and litterfall material was collected monthly for three years. The litterfall materials taken from the field were separated into their components (leaf, branch, bark, miscellaneous) in the laboratory, dried at 65 °C until they reached a constant weight and weighed. Afterwards, carbon analysis was performed on the milled samples. The amount of litterfall in one-hectare area was determined by using the conversion coefficient to hectares of the masses of the litterfall components collected from the traps. Then, these values were multiplied by the carbon concentration obtained as a result of the analysis, and the carbon stocks into forest floor through litterfall in a hectare area were calculated. The data were evaluated with variance, correlation and stepwise multiple regression analyzes. According to the results of the research, the amount of litterfall increased depending on the growth of the development stage and the total litterfall ranged between 3959 and 5698 kg/ha/year. The weighted carbon concentration of the litterfall was determined to be 50.3%. C stock, which enters the forest floor with total litterfall, varies between 1988-2857 kg/ha/year according to the development stages. Total litterfall in beech forests was estimated by stand characteristics, climatic characteristics and physiographic factors. Using the models obtained, the amount of annual litterfall can be estimated in the beech stands in the region and in similar sites. The findings of this research can be used in modeling studies, which are among the long-term goals of the Land Use, Land Use Change and Forestry sector.

Fase Reduced Graphene Oxide (rGO) dari arang tempurung kelapa melalui pemanasan baik menggunakan tungku maupun pembakar buatan telah berhasil dibentuk. Pemanasan dilakukan melalui 2 variasi temperatur yaitu 500 dan 1000ᵒC dengan waktu penahanan 5 jam. Pemanasan melalui pembakar buatan dilakukan dengan menggunakan bahan bakar minyak bekas yang dilengkapi termostat untuk mengukur suhu. Identifikasi fase dilakukan dengan menggunakan pengujian Xrays Diffraction Spectroscopy (XRD) dengan sudut 2θ yaitu 15-50ᵒ. Pola difraksi menunjukkan bahwa semua sampel memiliki fase rGO dengan nilai intensitas yang berbeda. Semakin tinggi suhu maka semakin besar nilai intensitasnya dibandingkan dengan sampel lainnya. Nilai intensitas ini menunjukkan peningkatan kristalinitas sampel akibat peningkatan suhu. Lebih lanjut, kristalinitas sampel juga berpengaruh pada nilai kekuatan beton normaldibuktikan dengan penurunan nilai kekuatan beriringan semakin meningkatnya nilai kristalinitas material.

This paper presents geochemical data for 171 core samples of the Carboniferous coal-bearing series and the Miocene cove from the central part of the Upper Silesian Coal Basin. Major oxide concentrations (Al2O3, SiO2, Fe2O3, P2O5, K2O, MgO, CaO, Na2O, K2O, MnO, TiO2, and Cr2O3) were obtained using XRF. Trace and major elements (Mo, Cu, Pb, Zn, Ni, Co, U, Cr, V, Mn, As, Th, Sr, Cd, Sb, Bi, Ba, Ti, W, Zr, Ce, Nb, Ta, Be Sc) were analysed ICP-MS. The main goals of this study were to demonstrate the distribution, as well as the stratigraphical variability, of the selected elements and to determine whether chemostratigraphy tools could be effectively applied to analyze Carboniferous and Miocene deposits of the USCB. Geochemical studies have shown showed different geochemical features of the samples from the Carboniferous and the Miocene. The diversity is mainly expressed in the enrichment of Miocene sediments in Ca and Sr related to biogenic carbonate material. It was also stated that the concentrations of trace elements associated with the detrital fraction, such as Zn, Cr, Co, Ba, Ti, Zr, Nb, and Sc show slightly higher values in Carboniferous sediments. On the basis of the content of Ti, Zr, and Nb, as well as ratios such as Th/U, Zr/Th, Ti/Zr, and TiO2/K2O, units with different inputs of the terrigenous fraction can be identified in both Carboniferous and Miocene formations. The paper shows that chemostratigraphy can be used as a stratigraphic and correlation tool for the Carboniferous and the Miocene deposits of the USCB. [ABSTRACT FROM AUTHOR]

Copyright of Indonesian Journal of Forestry Research is the property of Indonesian Journal of Forestry Research and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)

Copyright of Gazi Üniversitesi Fen Bilimleri Dergisi Part C: Tasarım ve Teknoloji is the property of Gazi University and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)

Karasal ekosistemler içinde en önemli karbon havuzları ormanlardır. Özellikle orman alanlarındaki canlı biyokütle ve orman toprağı yoğun miktarda karbon depolamaktadır. Biyokütle miktarları meşcere tiplerinin hektardaki ağaç serveti verilerinden hareketle belirlenmektedir. Bu çalışmada biyokütle verisinin doğruluğunu artırmaya yönelik ağaç kapalılık yüzdesi haritası ile çakıştırılması yapılmış ve nihai biyokütle haritası elde edilmiştir. Biyokütle haritası ve topraktaki organik karbon miktarları da uydu görüntülerinden belirlenerek Düzce ilinin karasal karbon stoğu ortaya koyulmuştur. Çalışma alanında ağaç türü bazında en fazla biyokütle ve karbon birikimi Kn ağaç türünde ve toplam biyokütle ve karbonun yaklaşık ¾’ünü depoladığı belirlenmiştir. En düşük biyokütle ve karbon miktarı ise Düzce’deki yayılışı sınırlı olan Çm ağaç türünde tespit edilmiştir. Orman alanlarındaki toplam karbonun %69.7’si canlı biyokütlede depolanırken, %30.3’ü ise toprakta depolanmıştır. Orman dışı alanlardaki özellikle toprakta tutulan karbon miktarları da değerlendirildiğinde tüm karbonun %84.6’sı orman alanlarında depolanırken, %14.5’lik kısmı ise tarım alanlarındaki toprakta ve % 0.9’luk kısım da diğer arazi sınıflarında depolanmıştır. Orman ve orman dışı alanlar birlikte değerlendirildiğinde toplam depolanan karbon miktarının %41’i toprakta depolanırken, %59’u ise canlı biyokütle üzerinde depolandığı belirlenmiştir.

The objective of this study is to investigate the effects of representative land use types and land cover (LUT/LC) of heavily deforested areas on soil properties in semi-arid region of Türkiye. Some of the soil properties have been measured on a grid with a 50 m sampling distance on the top-soil (0-15 cm depth). Data has been analyzed by using Ordinary Kriging/Spherical geostatistical model. Results indicated that the soil properties differed in terms of organic carbon (SOC), pH, bulk density, and the amount of sand, depending on the land uses in the study areas. The SOC concentration of top-soil layers has referred a significant difference (P

Copyright of Journal of Polytechnic is the property of Journal of Polytechnic and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)

In this study, carbon-based semiconductor technology was developed from tea waste biomass as a renewable, environmentally friendly and sustainable carbon source instead of fossil-sourced carbon, and a PN hetero-junction was formed with a P-type carbon layer on an N-type silicon substrate. The structure have the traditional diode characteristics, with a reverse saturation current Is=0.035 µA and ideality factor n=14.08. The large value of the ideality factor is attributed to the large series resistance in the structure. Additionally, it was demonstrated that that tea wastes can be considered as a technological product as a carbon source. [ABSTRACT FROM AUTHOR]

Copyright of Duzce University Journal of Science & Technology is the property of Duzce University Journal of Science & Technology and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)

Copyright of Artvin Çoruh Üniversitesi Orman Fakültesi Dergisi is the property of Artvin Coruh University and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)

In this study, the dynamism of forest areas was tried to be determined by determining the ecological differences between the areas where Fagus orientalis Lipsky. (Eastern beech, Fagaceae), a very important species for forestry in Turkey, and the soils of agricultural fields. lime %, total salt %, pH, texture, field capacity %, C%, N%, C/N ratios, 30-day carbon mineralization of the lands of Eastern beech forests and agricultural fields, which are naturally formed in Sivas province Koyulhisar district, under controlled conditions (28°C, 80 humidity %) was determined by the respiration method, and two areas in two different ecosystems were compared. When the carbon mineralizations of eastern beech soils were examined seasonally, it was determined as 19.54>18.23>17.87>17.18 mg C(CO2)/100g DS/30 day in spring>autumn>summer>winter seasons, while it was determined as 14.46>13.87>13.68>13.65 mg C(CO2)/100g DS/30 day in autumn>summer>spring>winter seasons in agricultural soils, respectively. Significant relationships were found between the C%, N%, 30-day carbon mineralization cumulative values and % carbon mineralization rates between both areas.

Our country has a great importance in the world market in terms of the production of metal raw materials and end products, especially in the iron and steel industry. In order to realize an efficient and high quality production process, it is necessary to continuously monitor the Carbon (C) and Sulfur (S) concentrations of the material throughout the entire production process. During the marketing phase of the products in question, the material qualities must be reported by the conformity assessment bodies. At this stage, it is expected to increase the accuracy and reliability of the measurement results in the quality control tests of the products. For this purpose, the verification and validation of the analysis method which were employed should be carried out by the conformity assessment bodies. However, it is observed that there are different applications that fall outside the procedures described in the relevant international guidelines. In this study as an example to the best available techniques, method validation and uncertainty estimation studies were carried out for the total carbon (C) and total sulfur (S) analyses in metals and alloys following the procedures described in the standard of "General Requirements for the Competence of Test and Calibration Laboratories". [ABSTRACT FROM AUTHOR]

Copyright of COMU Journal of Agriculture Faculty / ÇOMÜ Ziraat Fakültesi Dergisi is the property of Canakkale Onsekiz Mart University and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)

Time indications for the correlation and calibration of the Rotliegend of Germany are integrated and presented in a new way. The correlations are based on the visual balance of bio- and ecostratigraphic indications and radio-isotopic age determinations (RIA), whereby confidence limits, equivalent to those of the RIA, are applied also for other time indications (conchostracans, aquatic tetrapods, fishes, insects, macroflora, and ecostratigraphic indications). In contrast, terrestrial tetrapods and their tracks, chemo- and sequence stratigraphy, and magnetic susceptibility did not contribute to correlations in the Rotliegend in Central Europe. The Illawarra Reversal of the Earth' magnetic field (≈ 265 Ma) is fundamental for correlation and calibration. In general, however, the Regional Stratigraphic Scale is calibrated using U-Pb CA-ID-TIMS-RIA on zircon, Ar-Ar- and Rb-Sr-based RIA and, in addition, in the Early and Late Rotliegend using orbital-climatically controlled eccentricity cycles (≈ 100 ka, ≈ 400 ka). The boundary ages of the subgroups and of most formations are rounded to 0.5 Ma to avoid overinterpretation. Because of some inconsistent time indications alternative interpretations are also offered. The hitherto differing ages for the global Carboniferous-Permian boundary are the result of different dating methods: The ≈ 296 Ma in the Stratigraphic Tables of Germany 2002 and 2016 A (STG 2002; STG 2016 A) is an integrative age based on RIA from Central Europe, whereas the ≈ 299 Ma in the Global Stratigraphic Scales 2004 ff. and the STG 2016 B is based on a CA-ID-TIMS RIA on zircon from the southern Ural area. The age of ≈ 299 Ma is plausible from the perspective of the current Rotliegend RIA because the Rb-Sr age of 290.7 ± 0.9 Ma for the Donnersberg Formation (Lippolt & Hess 1989) has been replaced by the age of 294.5 ± 2.2 Ma, as recalculated in the present work. The updated time scale developed here will be integrated in the Stratigraphische Tabelle von Deutschland Kompakt 2022 (STDK 2022) and into the Stratigraphic Table of Germany Compact 2022 (STGC 2022). The age of the base of the Rotliegend in the Saar-Nahe Basin (SN, base Remigiusberg Formation and Glan Subgroup) is ≈ 299 Ma (U-Pb CA-ID-TIMS, zircon) resp. ≈ 300 Ma (Ar-Ar); the balanced compromise age of both is ≈ 299.5 Ma. In the Thüringer Wald (TW), the Rotliegend begins with the Ilmenau Formation (Subkommission Perm-Trias 2011) at ≈ 299.5 Ma (U-Pb CA-ID-TIMS). On the Flechtingen Block, at the southern margin of the Central European Basin, the oldest volcanic rock of the Altmark Subgroup is dated at 302 ± 3 Ma (U-Pb SHRIMP data). Accordingly, the Rotliegend in the STG 2002 and STG 2016 A starts at ≈ 302 Ma. However, the mean age calculated in the present work for the SHRIMP data of Breitkreuz & Kennedy (1999) is 298.6 ± 1.9 Ma, so that the base of the Altmark volcanic succession is here re-dated as ≈ 300.5 Ma. Thus, the ages of the present lithostratigraphic lower limits of the Rotliegend in northern Germany (CEB), in the TW and in the SN are, with ≈ 300.5 Ma to ≈ 299.5 Ma, only weakly diachronous if the nominal (face) values, which are both in the latest Carboniferous, are compared without the confidence intervals. For the first time, the Rotliegend of Germany is geochronologically subdivided into Early (≈ 300.5-295.5/294 Ma), Middle (≈ 295.5/294-266 Ma) and Late Rotliegend (≈ 266-257.5 Ma). The very long lasting Middle Rotliegend includes numerous and also extremely long stratigraphic gaps as a result of the amalgamation and the associated immense uplift of Pangaea in the area of Central and Western Europe. A very large stratigraphic gap in the Central European Basin (CEB) of ≈ 15 Ma (≈ 281-266 Ma, here called the Pangaea Gap) is supported by conchostracans, the Illawarra Reversal and the different palaeomagnetic properties of the sediments below and above the gap, which are discussed here for the first time. The Middle Rotliegend (duration of ≈ 29.5/28 Ma) is approx. twice as long as the Early (≈ 5.5/7 Ma) and Late Rotliegend (≈ 8.5 Ma) combined. The latter, however, contain the thickest successions in the Saar-Nahe Basin and the Central European Basin, respectively, which are free of gaps in the basin centre, with 'gaps' being defined in this context as time spans of ≤ 100 ka and ≤ 400 ka, respectively. In the CEB, the Elbe Subgroup is cyclostratigraphically calibrated to 5.6 Ma. A gapless area in the Saar-Nahe Basin is the Glan Subgroup, which covers only 4 Ma and 3 Ma, respectively; correspondingly, its subunits G1 to G10 (Glan 1 to Glan 10), introduced here, last on average 0.4 Ma and 0.3 Ma, respectively. This results in a maximum accumulation rate of 870 Bubnoff (Bub, m/Ma, mm/ka) and of 1150 Bub, respectively, which can be explained by a maximum of tectonic activity along the Hunsrück Southern Border Fault. For the lower Nahe Subgroup (N1 to N5, Nahe 1 to Nahe 5), the maximum accumulation rates are ≈ 450-200 Bub and for the upper Nahe Subgroup (N6-N8), at an estimated duration of 12 Ma ≈ 125 Bub and ≈ 50 Bub at a duration of 30 Ma, respectively. In the Central European Basin the maximum accumulation rates are much lower compared to the Glan Subgroup, with 200 Bub in the Elbe Subgroup and ≈ 360 Bub in the Havel Subgroup (Fig. 27), although here the subsidence rate may have been higher than the accumulation rate, as the basin was ≈ 130 m below sea level at the end of Folge ro4 (Top of the Hannover Formation; this paper). We recommend (1) Bubnoff (Bub) as unit of measure of the accumulation rate and (2) the stratigraphic terminology of the Subkommission Perm-Trias (2011) and the STG 2016 A. We here propose that numerous tuffs of the Glan Subgroup could originate from volcanic centres of the TW, whereas so far only source areas south of the SN were discussed: On the one hand, the tuff-rich time of the upper Jeckenbach Subformation - Odernheim Formation (= Glan units 7 and 8 = G7/G8) seems to correlate with the volcanogenic Oberhof time in the TW and, on the other hand, the tuff-poor time of the Wahnwegen Formation - middle Jeckenbach Subformation (G2/G6) seems to correlate with the upper Ilmenau, Manebach, Goldlauter and lowest Oberhof formations, which are devoid of volcanic rocks in the TW. Should causality exist here, an additional and also precise criterion for correlation would be established. At present there are two variants: On the one hand, volcanism in the Oberhof Formation, according to RIA (U-Pb CA-ID-TIMS on zircon), begins ≈ 1.8 Ma earlier and ends ≈ 0.8 Ma earlier than in the Donnersberg Formation (Ar-Ar, Rb- Sr recalculated). On the other hand, the conchostracan Lioestheria pseudotenella in the TW, if considered equivalent to L. cf. pseudotenella in the SN, the ecostratigraphic and lithofacial indications and the aquatic tetrapod D. pulcherrimus, point to for a similar age of these magmatites. The Sobernheim Lens (SN, Nahe units N4/N5) with its fossils so important for correlations is here assigned to the Jakobsweiler Member (N4, upper Donnersberg Formation), to the Quartzite-Conglomerate (N5, in literature often Wadern) and to the lowermost Standenbühl Formation (N4/N5). The youngest time indication Co13, the conchostracan Lioestheria arroyoensis sp. nov. correlates the upper Standenbühl Formation (N8, Martens 2020, where N8 may be extremely long), roughly with the Arroyo Formation in Texas (≈ early Kungurian). The here favoured age of the Tambach Formation of ≈ 294-292 Ma is significantly higher than the ≈ 286-283 Ma of STG 2016 A and the ≈ 284-281 Ma of STG 2016 B. It is based on RIA R25 (Table 9; lower Rotterode Formation, 295.8 ± 0.4 Ma; Lützner et al. 2021), which is the youngest CA-ID-TIMS RIA in the TW, and the duration estimate of the Rotterode - Tambach gap. In the SN, the youngest RIA R29 (Rb/Sr) is from the Donnersberg Formation (294.5 ± 2.2 Ma, this paper). From here on until ≈ 265 Ma (Illawarra Reversal), the numerical ages of all Rotliegend units and their connection to the Global Stratigraphic Scale (GSS) are uncertain and therefore correlations between Central Europe and the global reference section in the southern Ural area, partly biostratigraphically via North America, vary greatly. In this contect, the „series“ Wolfcampian and Leonardian (standard Permian units of the USA) played an important role. However, these lithostratigraphic units are at least unsuitabel as a reference system for large parts of North America, because they represent very variable time spans from region to region, similar with the "Lower Rotliegend" ("Autun") and "Upper Rotliegend" ("Saxon") of Central and Western Europe and therefore their assignement to the GSS is also very variable. This is due, among other things, to the fact that the Wolfcampian is often still understood as "lower Lower Permian", although considerable parts of it are now placed in the Carboniferous, because as a result of the introduction of the Global Stratigraphic Section and Point (GSSP) for the base of the Asselian Stage (= global base of the Permian in the southern Ural area), the conventional regional Carboniferous-Permian boundaries shifted to an higher stratigraphic level and thus to a younger age in the USA, China and the Donbass (Fig. 14). If the 57 sedimentary cycles in the Ottweiler and Glan subgroups (Königer & Stollhofen 2001: mean duration 245 ka each) in the SN are orbital-climatically induced, these cycles can only be 100 ka cycles (short eccentricity). This is also supported by the 6 cycles in units G7 and G8 that have been described in detail in the literature, which are consistent with the duration of the Glan Subgroup of 3 Ma and (preferred) 4 Ma, respectively. The total duration to be expected from 57 cycles à ≈ 100 ka is ≈ 5.7 Ma in contrast to the duration determined here according to RIA of ≤ 8 Ma. One reason for the difference could be that in the Ottweiler und Glan subgroups there are cycles that have not been recorded so far. The time span of ≤ 8 Ma is also an outcome of the new estimate for the duration of the Cantabrian Gap (early Stephanian) in the Saar-Nahe Basin of ≈ 3.6 Ma that is clearly longer than proposed in the STG 2002 and STG 2016. [ABSTRACT FROM AUTHOR]

Copyright of Ege Üniversitesi Ziraat Fakültesi Dergisi is the property of Ege Universitesi, Ziraat Fakultesi and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)