Ultimate Source Research Articles

Ayurvedic concept of Manas (mind) in perception of knowledge

Maintenance of health is given prime importance in 'Ayurveda', for that both physical and mental factors are equally important, because the mind act in conformity with the body and the body acts in conformity with the mind. mind is not visible. Any kind of perception and functioning of sensory or motor organs is indicative of presence of mind. Without mind executing as a mediator between external as well as internal environment, soul does not acquire any perception. Ayurveda science strongly proposes mind as chief convener of all external and internal stimuli to body and a mediator for motor reactions to all these stimuli. If Mana is not doing it's duty, nothing is perceived. mind has two properties, namely Anutva and Ekatva. Mind is the seat of pleasure (Sukha) and misery (Duhkha). Understanding the concept of mind is important because balanced state of mind is the ultimate source of health. mind, soul and body are the tripod on which life depends. Both body and mind are the resort of pleasure and disorders.

The Mediating Role of Organizational Climate in Assessing the Influence of Local Governance-Based Paternalist Leadership on Employee Innovation

Abstract With the acceleration of economic globalization and the increasing uncertainty in the external market environment, Chinese enterprises are increasingly required to survive and thrive through continuous innovation activities. As the ultimate source of organizational innovation, the staff determines the overall level of organizational innovation. Simultaneously, leadership behavior within an enterprise profoundly influences employees’ innovative behavior. Therefore, influencing employees’ innovative behavior through a leader’s conduct has become a hot topic of academic discussion. The study aims to explore the impact of locally based paternalistic leadership on employees’ innovative behavior and introduce organizational climate to examine the mutual influence between these two variables. This is a quantitative case study to be conducted on various banks in China, utilizing SPSS software and bootstrap mediator variable analysis. According to the results of this research, paternalistic leadership has a significantly beneficial impact on innovative employee behavior and organizational climate. However, the authoritarian leadership dimension negatively affects innovative behavior and organizational climate. Organizational climate has a substantially positive effect on innovation behavior, and organizational climate plays a role as a mediating variable in the influence of paternalistic leadership on innovative behavior. The future value of this research lies in providing practical suggestions for the development of leadership behavior theory and improving the efficiency of human resource management.

Structure and materials of alkaline fuel cell

To solve the problems of energy and environment, after experimentations and selections, hydrogen steps into the limelight; we call it "the ultimate energy source for the development of human society," and fuel cell technology is an essential step of pursuing the recyclable hydrogen energy. Fuel Cell is viewed as one of "The ideal power generation devices in the 21st century"; it has a high energy transformation efficiency, and the electricity generation process has a low environmental impact. If the fuel is being provided, fuel cells can continuously provide electricity, which can likely be applied in power plants, electric vehicles, electronic devices, mobile communications, and space facilities. This work focuses on Alkaline Fuel Cells. The oxidation-reduction process will be more straightforward in alkaline-based electrolytes than in acidic electrolytes, and the alkaline system will also perform better under room temperature. Besides, Alkaline Fuel Cells (AFC) can use non-platinum catalysts, so the cost is lower than the other Fuel Cells. Thus, designing a Hydrogen-based AFC is what's being focused on in this article. However, AFC has its disadvantages too. First, the CO2 in air and fuel gas must be cleaned up because of the alkaline electrolyte. Furthermore, water is a by-product of the electrochemical reactions inside AFCs. Therefore, AFC performance will be seriously affected if the water doesn`t expel. Another issue that current AFCs face is the problem of CO2 poisoning. To address the above questions, we approached it from a thermodynamic perspective, compared the basic structure, material, drainage method, etc., of multiple alkaline fuel cells, and selected the more efficient ones that will be more effective for developing the AFCs.

Miniature Fuel Cell with Monolithically Fabricated Si Electrodes- Application of a PDMS Flow Channel for Operando Observation -

Miniature fuel cells have attracted attention as an ultimate portable power source, and we have developed monolithically fabricated Si electrodes for the miniature fuel cells [1,2]. In the fuel cells, two Si electrodes with porous Pt catalyst layer are pressed onto either side of a PEM (polymer electrolyte membrane) , and the prototype fuel cells showed promising performances of over 500mW/cm2 output at 313K with H2-O2. However, the high output was obtained with only small reaction area. Along with enhancement of the reaction area, the performance dropped. We assumed that the performance drop is caused by flooding due to increased water production, which was ignored because MEMS fuel cells are dimensionally small and the outputs are also small. In this study, we attempted to observe the behavior of produced water on the fuel flow channel using a novel transparent channel cover as shown in figure 1. Furthermore, it was assumed that the produced water stays in the concave portions on the catalyst layer, and stripe-shaped projections were formed on the channel cover to prompt drainage of the produced water from the fuel channels.The transparent fuel channel cover was fabricated with PDMS using soft lithography techniques. Initially, a mold for the cover was made with a dry film resist. Micro stripe pattern with 40μm width were made. Considering the PDMS shrinkage during polymerization, the mold pattern had to be formed a few percent larger than the desired shape. Figure 2 shows the whole view of the PDMS channel cover on a miniature fuel cell with Si electrodes. The reaction on the Si substrate was 1mm and 4mm long. Within the area, 100μm x 100μm sections were etched down to the backside catalyst layer. Magnified view on the reaction area is shown in figure 3. It was found that the stripes were finely aligned on the concave portions on the Si electrode.Figure 4 shows the polarization curves of the power generation tests. Results with the novel fuel channel cover with stripes showed higher output compared to the conventional simple cuboid straight shape cover. Figure 5 shows the microscopic view of the channel. While produce water droplets were observed on downstream area in the conventional cuboid shape channel, no droplets were observed with the novel channel cover. It was assumed that drainage of the produced water was successfully prompted and smooth fuel supply to the catalyst layer was realized by the novel fuel channel cover. Acknowledgement This work was partly performed under the Cooperative Research Program of “NJRC Mater. &Dev.” References [1] M. Kobayashi, T. Suzuki, M. Hayase, Journal of Power Sources, 267, 622-628 (2014).[2] R. Shirai, et al., Journal of The Electrochemical Society, 166(15), D834 (2019) Figure 1

The Cross and Our Calling

Redeemer University is a Canadian Christian university located in Ancaster, Ontario. Founded in 1983 in the Reformed Christian tradition, Redeemer’s mission is to prepare students to join Christ in his redemptive work through their careers and callings, while also fostering faculty research and scholarship in every discipline from a Christian perspective. Over the past forty years, Redeemer has evolved from a small college with limited degree granting authority to a full university offering a variety of programs including a B.A., B.Sc., B.Ed., B.B.A., B.Kin., and B. Comms. Redeemer currently faces challenges stemming from a post-Christian Canadian culture and the impact it has had on widespread individual belief in the psychological self as the ultimate source for personal identity and understanding. The changing higher education marketplace also contains a proliferation of degree granting institutions, and students are increasingly seeking clear and direct pathways to careers, making institutions like Redeemer with traditional degree nomenclature to appear less relevant and desirable. However, some of these challenges also present opportunities. Post-Christian culture also means that more Christians desire a unique, faith-based higher education institution, as it becomes more difficult to express faith in public spaces.

Feedback strategies in distance education: a survey of university students

Abstract Screen-mediated teaching at the university level has necessitated a redesign of learning environments across various dimensions, encompassing epistemological, relational, and pragmatic aspects. How can the Digital Learning Ecosystem nurture these dimensions? Does the ecosystem initiate a feedback loop between the teacher and the student, configured not only as an evaluative process but also as a reflective and adaptive one? The feedback loop holds a generative value; it triggers an internal process in the student, enabling them to construct knowledge about their ongoing activities and comprehend through their own evaluative acts. Students stand as the ultimate source of all feedback; they are the ones who ultimately generate it, and it is this process that catalyzes learning. Feedback strategies further promote alignment between the teacher and the student, fostering continuous redesign and co-design. The paper aims to present a survey collecting students’ perceptions on the condition of separation between professors and students during distance learning and activation of the educational relationship and feedback through digital devices.

Detrital gold morphology and recycling around the early Miocene St Bathans paleovalley, Central Otago, New Zealand

ABSTRACT The St Bathans paleovalley developed as a major southwest-draining fluvial system during early Miocene rejuvenation of the Central Otago landscape. Rounded quartz pebbles and detrital gold were recycled from Eocene quartz pebble conglomerates into the headwaters of this Miocene paleodrainage system on the northern margin of the Otago Schist belt. Gold particle morphology is mostly irregular and rough, locally with relict gold crystal shapes, plus a minor component of well-defined flakes. Incremental rounding and surface deformation at the 10 µm scale has occurred through several recycling events in Central Otago, hindering linkage of Miocene and younger placer gold to ultimate basement sources. More intense deformation of the gold, forming thin flakes, occurred in the lower reaches of the Miocene paleodrainage system as gold was transported >100 km to eastern Southland. Hence, the St Bathans paleovalley has been an important source of gold for historic mining in Central Otago and Southland.

The mobility of copper, zinc, molybdenum, and tungsten in subduction zone fluids

Porphyry-type ore deposits are closely associated with subduction zones, but the ultimate source of the metals in these deposits is still uncertain. To test whether aqueous fluids from the subducted slab may contribute to the metal enrichment, we investigated the partitioning of Cu, Zn, Mo, and W between saline aqueous fluids and the subducted basaltic crust at 2.5–3.0 GPa and 650–670 °C by experiments in piston cylinder presses. The bulk fluid/solid partition coefficients (Dfluid/solid) of Cu and Zn increase significantly with fluid salinity. For Cu, Dfluid/solid is less than 1 in a salt-free aqueous fluid, but at a salinity of 10 wt% NaCl, Dfluid/solid approaches 10. On the other hand, the Dfluid/solid of Zn is still below 0.4 even at the same salinity. Dfluid/solid of Mo is always relatively high (>4), with only a very slight enhancement by salinity at 2.5 GPa. The fluid/solid partition coefficient of W is close to 1 for a chloride-free fluid, but slightly decrease with increasing salinity. Overall, these experimental data show that saline aqueous fluids released from the basaltic layer of the subducted oceanic slab can effectively transport Cu and Mo and therefore enrich these two metals in the mantle wedge. This enrichment does not contradict the observation that Cu concentrations in primitive arc magmas and MORB are similar, since these concentrations may be controlled by a buffering sulfide phase. The enrichment of copper in the source then does not necessarily increase Cu concentrations in the melt, but it ensures that the copper-bearing sulfide phase is not exhausted during repeated melting events. For molybdenum, our data suggest that aqueous fluids from the slab are the major source of Mo in arc magmas. Due to the high pre-enrichment of Mo in some sediments, there may be a direct link between the types of subducted sediment and the location of porphyry Mo deposits. On the other hand, the contribution of slab fluids to the Zn budget of these magmas is likely negligible. The W partitioning data are consistent with isotopic evidence for the mobility of W in subduction fluids. Moreover, the behavior of Mo and W is strongly affected by the abundance of rutile in the solid residue. In a rutile-free lithology, not only Mo, but also W would strongly partition into the fluid. As some sediments may be highly enriched in W relative to the average mantle, fluids from such sediments may also produce a significant W enrichment in the mantle wedge, provided that the sedimentary residue is free of rutile.

From Laozi to Lao-Zhuang and Huang-Lao Daoism: The Two Paths of Oneness in the Development of Early Daoist Thought

This paper proposes examining the central notion of Oneness (一 yi) in Daoist thought by offering an analysis of its uses in the early writings of the Daoist tradition, beginning with the Laozi 老子 and the Zhuangzi 莊子 before moving on to Huang-Lao 黃老 texts. While Oneness in the Laozi primarily appears as another “name” for Dao, it was used in discussions of cosmogony and cosmology, political governance, and personal cultivation. These multiple aspects of Oneness in the Laozi were later developed along two different paths in Daoist thought. The first, exhibited in the Zhuangzi, the Baopuzi 抱樸子, and other similar documents, treated Oneness as the ultimate source of all things and extended its meaning in the context of personal cultivation. In resonance with this path, their central teachings concerned “maintaining Oneness” (守一 shou yi). In the second path, expressed in the Huang-Lao tradition’s understanding and interpretation of the Laozi, Oneness acquired a certain concreteness and was singled out as the criterion and standard for social order, while the notion of Dao gradually devolved into abstraction. Huang-Lao writers hence emphasized Oneness in the sense of unification, uniformity, a singular decree, or law, which opened a theoretical gap between Oneness and Dao, and their central teachings concerned “utilizing Oneness” (用一 yong yi) and “holding Oneness” (執一 zhi yi).

Detrital zircon and tourmaline unravel polycyclic provenance of sedimentary infill of the Cretaceous Tupanciretã formation, southern Brazil

The recognition and evaluation of polycyclic processes in sedimentary units are critical for proper provenance analysis and sedimentary system interpretation. The chemical composition and textural maturity of detrital tourmalines and zircons allow identification of sediment source areas, transport, and deposition. This study investigates the origin and history of post-Gondwanan sediments of the Tupanciretã Formation in southern Brazil, which lacks provenance studies. The Tupanciretã Formation is in a similar setting of the Bauru Supersequence at the uppermost portion of the Paraná Basin. Detrital zircon ages indicate sediment provenance from the Transamazonian, Grenvillian, and Brasiliano orogenic cycles of the Rio Grande do Sul Shield and younger grains (280-128 Ma) record contribution from the Choiyoi and Serra Geral igneous events, with a maximum deposition age of 127 Ma. Detrital tourmaline chemical analyses points to the Sul-riograndense Shield as the ultimate source, with metapelitic, metapsamitic and granitic origins. The predominant degrees of roundness are well rounded to rounded suggest evidence of sediment recycling from sedimentary units of the Paraná Basin, with important aeolian reworking involved. Zircon U–Pb signatures are compatible with the eastern sector of the Botucatu Formation in Rio Grande do Sul as the immediate source and the northeastern Sul-riograndense Shield as the ultimate source. Intermediate sources between the Sul-riograndense Shield and the Tupanciretã Formation were Gondwanan sedimentary units of the Paraná Basin, with possible participation from the Camaquã Basin.

Experimental investigation on the interaction characteristics of lead‑bismuth liquid metal and water

The energy conversion and utilization of liquid metals is becoming one of the effective ways to solve energy problems. The conversion and transfer of thermal energy from liquid metals to water are significant in advanced nuclear energy and metallurgy. It has been an urgent concern, especially in Generation IV of advanced nuclear energy systems‑lead-cooled fast reactors and the ultimate energy source for humanity-fusion engineering. In this paper, a large-scale liquid metal and water interaction test platform was developed to investigate the lead‑bismuth liquid metal and water interaction and the cover gas pressurization characteristics. Firstly, the evolution of phase behavior and water/vapor migration paths were inferred based on the transient temperature law. Secondly, the cover gas pressurization patterns above the molten pool were analyzed, and the test data showed three pressurization patterns, including two types of local vapor explosions. Additionally, this paper predicted the existence of another dangerous pressurization mode, i.e., overall vapor explosion. Finally, the cover gas pressurization rate model was established, and there is an appropriate matching between the model and test data with an average relative error of 12.6%. This paper provides an essential reference for profoundly understanding the energy conversion and thermal interactions between liquid metals and water.

Origins and evolution of two types of Late Triassic granitic magmas in the Caolong-Xiangkariwa area of central-eastern Songpan-Ganze terrane, northern Tibet: Implications for pegmatite lithium mineralization

Pegmatite-type lithium (Li) deposits are an important source of the low-carbon energy metal, which is generally considered to be formed by the high degrees of differentiation of strongly peraluminous granitic magma. However, the question of whether the parental rocks of these peraluminous magmas are igneous or sedimentary has been widely debated. Recent studies have identified a world-class pegmatite-type Li deposit belt (up to 2800 km long) closely associated with the Late Triassic granitoids and (meta)sedimentary rocks along the West Kunlun and Hoh Xil-Songpan-Ganze terranes in northern Tibet. This study presents a comprehensive petrological, geochronological, and geochemical study on the two types of Late Triassic granitoids in the Caolong-Xiangkariwa area of the Yushu region of central-eastern Hoh Xil-Songpan-Ganze terrane in northern Tibet: type A includes the Tongtianhe-Zhenqin-Zhaduo-Zhaya-Xiangkariwa (TZX) diorites and granodiorites (218−212 Ma), and type B includes the Caolong two-mica and muscovite granites (213−205 Ma), as well as ore-barren, beryl-bearing, and spodumene-bearing pegmatite dikes (209−196 Ma). The TZX diorites and granodiorites contain variable amounts of amphibolite and biotite. They are metaluminous to slightly peraluminous with variable SiO2 (54.4−71.3 wt%), MgO (0.72−7.26 wt%) contents, and Mg# values (40−70). Some samples with low SiO2 (54.4−58.5 wt%) contents have geochemical features similar to high-Mg andesites: e.g., high MgO contents (5.24−7.26 wt%) and Mg# values (61−70). The TZX diorites and granodiorites exhibit less enriched (86Sr/87Sr)i (0.7080−0.7118) and εNd(t) (−4.8 to −8.0). By contrast, the Caolong two-mica and muscovite granites are characterized by the occurrence of abundant muscovite (plus tourmaline and garnet) and are strongly peraluminous. The Caolong granites and pegmatites are geochemically characterized by high SiO2 contents (68.8−79.8 wt%) and low MgO contents (0.01−0.10 wt%) and Mg# values (4−23). They have εNd(t) values (−8.8 to −11.4; granites: −8.8 to −10.8; pegmatites: −9.2 to −11.4) that are more enriched than the TZX diorites and granodiorites but similar to those of Songpan-Ganze (meta)sedimentary rocks (−7.4 to −12.9), and the Caolong two-mica granites have high zircon δ18O values (11.6−12.1). In addition, decreasing K/Rb ratios correspond to increasing Cs contents in K-feldspar and muscovite from the Caolong granites and pegmatites. Taking into account the Late Triassic granitoids and (meta)sedimentary rocks in the Hoh Xil-Songpan-Ganze terrane, we suggest that the TZX diorites and granodiorites were most probably formed by the partial melting of metasomatized lithospheric mantle that subsequently underwent extensive fractional crystallization. Conversely, the Caolong two-mica and muscovite granites were likely generated purely by the partial melting of (meta)sedimentary rocks rather than via the evolution of dioritic-granodioritic magmas. In summary, there were two kinds of granitic magmas with different sources in the Caolong-Xiangkariwa area. Finally, the Caolong pegmatites were most likely formed by the extreme differentiation of two-mica granitic magmas rather than the dioritic-granodioritic magmas. Therefore, the evolution of magmas derived from (meta)sedimentary rocks were most likely to have formed the Li-rich pegmatites. Moreover, these (meta)sedimentary rocks representing the ultimate Li source must have undergone strong chemical weathering, resulting in significant Li enrichment.

Effects of season and slope orientation on stable isotopes of different water bodies in the subalpine shrub zone of the eastern Qilian Mountains in China.

The subalpine shrub zone of the Qilian Mountains is an important water-retaining area, and it is crucial to clarify the processes of its hydrological cycle. Therefore, based on the stable isotope values of different water bodies in the subalpine shrub zone of the eastern Qilian Mountains from May to October 2019, the characteristics of δD and δ18O of different water bodies and their hydraulic relationships with each other were studied. The results showed that the stable isotope values of precipitation exhibited the largest fluctuations, while they were the most stable for groundwater. Plant transpiration was stronger than the evaporation of other water bodies. The stable isotope of precipitation was enriched in high temperature and low humidity environments. Isotopic values of plant and soil water were higher and more stable on the semi-sunny slope than on the semi-shady slope. According to the stable isotopes, there was a strong hydraulic relationship between the different water bodies in the study area, and precipitation was the ultimate source of all of them. Precipitation replenished soil water through infiltration. Part of the soil water was absorbed by plants, while the rest continued to infiltrate to replenish groundwater. Groundwater and precipitation replenished the river water.

The Singhbhum Craton (India) records a billion year of continental crust formation and modification

The petrogenesis of continental crust from its ultimate mantle source can be reconstructed from the element abundances and radiogenic isotope compositions of ideally pristine igneous rocks. The initial isotope compositions of igneous rocks provide geochemical constraints on the age, composition and evolution of their source(s). Determining initial isotope ratios for rock samples can be challenging, especially in rocks with a long and protracted thermal history. The Rb-Sr system is highly sensitive to parent-daughter element fractionation during magma differentiation. This makes the Rb-Sr isotope systematics ideal to trace the precursor composition of Archean felsic crust and constrain the time of element fractionation during the formation and subsequent modification of continental crust. Initial isotope compositions can be obtained directly from minerals that strongly prefer the daughter element and effectively exclude the parent element of the radio-isotope system of interest. Apatite, having a near zero Rb/Sr ratio, is ideal for preserving its initial 87Sr/86Sr and zircon records initial 176Hf/177Hf compositions. Combined modelling of Sr and Hf isotope data from granitoids of the Archean Singhbhum Craton, indicates that the older Paleoarchean granitoids, emplaced between 3.53 Ga and 3.44 Ga, were derived from a mafic precursor (∼52–54 wt% SiO2) sourced from a depleted mantle at ∼3.71 Ga. Initial 87Sr/86Sr isotope signatures of matrix apatite and apatite inclusions in zircon from the younger Paleoarchean granitoids (3.4–3.2 Ga) of the Singhbhum Craton indicate these younger granitoids were produced by mixing of magma generated from an older mafic source and partial melts derived from the older granitoids. The combined Sr-Hf isotope modelling links the timing of mantle extraction of the precursor material for Paleoarchean Singhbhum granitoids with a known mafic crust extraction event at ∼3.71 Ga. In combination, the new Sr isotope data from apatite combined with whole rock and zircon Hf isotope data from the literature reveal a ∼1 Ga protracted crustal growth and differentiation history of the nucleus of the Singhbhum Craton. By combining radio-isotope systems like 87Rb-87Sr and 176Lu-176Hf, the petrogenesis of Archean felsic crust from the extraction of mafic material from the mantle to reworking in an orogenic cycle to emplacement can be reconstructed. This approach can be applied to other greenstone-gneiss terranes to quantify the spatio-temporal and compositional evolution of voluminous felsic crust and the formation of cratons in the Archean.

Evidence of site-specific and male-biased germline mutation rate in a wild songbird.

Germline mutations are the ultimate source of genetic variation and the raw material for organismal evolution. Despite their significance, the frequency and genomic locations of mutations, as well as potential sex bias, are yet to be widely investigated in most species. To address these gaps, we conducted whole-genome sequencing of 12 great reed warblers (Acrocephalus arundinaceus) in a pedigree spanning three generations to identify single-nucleotide de novo mutations (DNMs) and estimate the germline mutation rate. We detected 82 DNMs within the pedigree, primarily enriched at CpG sites, but otherwise randomly located along the chromosomes. Furthermore, we observed a pronounced sex bias in DNM occurrence, with male warblers exhibiting three times more mutations than females. After correction for false negatives and adjusting for callable sites, we obtained a mutation rate of 7.16 × 10-9 mutations per site per generation (m/s/g) for the autosomes, and 5.10 × 10-9 m/s/g for the Z chromosome. To demonstrate the utility of species-specific mutation rates, we applied our autosomal mutation rate in models reconstructing the demographic history of the great reed warbler. We uncovered signs of drastic population size reductions pre-dating the last glacial period (LGP), and reduced gene flow between western and eastern populations during the LGP. In conclusion, our results provide one of the few direct estimates of the mutation rate in wild songbirds and evidence for male-driven mutations in accordance with theoretical expectations.

Duyguların Günlük Yaşama Yansımaları: Pozitif Duyguların İşlevselliği

People by nature tend to experience more positive emotions and less negative emotions. For centuries, philosophers have stated that happiness is the ultimate source of human motivation. Therefore, many individuals think that the more positive emotions they experience, the happier they will be, and they strive for it. Many different situations such as socioeconomic level, educational status, gender, culture affect the level of happiness of individuals, but the desire to be happy is present in every segment. The endless pursuit of happiness can often lead to unrealistic expectations and some psychological problems in the face of life events. The increase in positive emotions can open up more space for the person to learn, think and develop together with happiness. However, positive emotions do not consist of happiness, but there are also different emotions that contribute to happiness and nourish the person. The positive emotions experienced by the person in daily life are important in terms of better performance and healthier relationships. In this respect, when we look at the literature on this subject, it has been seen that there is a gap in the studies conducted in Turkey. Emotions are important determinants of behavior. Any risky behavior that may arise can be harmful to both the individual and the society. Emotion regulation also affects behavior positively. For this purpose, the aim of this study is to deal with positive emotions, which have not been discussed before, in a theoretical dimension, to adapt these emotions to daily life, to increase the resources that the person has and to convey their reflections on the lifestyle.

FISCAL POLICY OF UKRAINE AS THE FACTOR OF THE SUSTAINABILE DEVELOPMENT OF THE TERRITORIES IN CONDITIONS OF MARTIAL LAW

It proves that the fiscal policy in the war conditions needs economic diversification with the help of the use of existing resources optimization and the search of uninvolved ones as well. The aim of the research is to deeply analyze the theoretical-methodological bases of Ukrainian fiscal policy formulation and fulfillment in conditions of martial law and its impact on the financial system of the government. Government’s revenue (taxes) and government’s expenditure are the main instruments of fiscal policy. High uncertainty in condition of full-scale war led to the reducing of the effectiveness of market instruments of fiscal policy and made it impossible in the traditional format.
 It defines that instruments of fiscal policy helped to provide some measures for designing expansionary fiscal policy in conditions of martial law. Grant funds of international partners as well as non-tax revenue at the expense of voluntary transfers from citizens, enterprises, and organizations to support Ukraine have become the ultimate source of government’s revenue from the beginning of the war. The search of instruments for financing (ensuring defense capability and security of the country; social expenses, increasing the monetary support of the military, debt service expenses) has become the key of fiscal policy.
 It explains that negative opening balance of consolidated budget of Ukraine targeted at cyclical economy position of the country proves the sharp softening of fiscal policy. The probation of such kind of fiscal policy was due to the intense growth of the budgetary expenditures on providing defense capabilities of the country and incentives to support economy in conditions of martial law.
 It proves that the abrupt deficit expansion of consolidated budget is the justified countercyclical measure of fiscal policy in conditions of martial law. The softening of fiscal policy in the country has mainly become possible because of quite balanced fiscal policy of past years and considerable international support as well.

Combination of Zero Waste Patterns to Maximize Multi Fabric and Wastra Nusantara Applications

The fashion industry has long been known as the ultimate source of waste in landfills. Many designers and fashion enthusiasts tried to introduce slower fashion to promote sustainability. Among many approaches, the zero-waste pattern (ZWP) has been known as the keyword that captures the attention of many. The baseline is to produce any fashion pieces with 15% waste or up to nearly 0% waste from a piece of cloth. Because of this definition, many designers are trapped into thinking that Zero Waste Fashion (ZWF) products should only use mono fabric. Indonesia has various local fabrics (wastra) that can be explored. The initial bottom line of wastra is to use the whole fabric with no cutting at all. Therefore, the same spirit of ZWF is found relatable to the use of wastra in the modern context. This study aims to find the right multi-fabric combination using zero waste patterns on wastra. This study uses a design thinking method with an experimental approach. The fabric used in this research is limited to plain modern fabric and wastra with the tie-dye technique. This study found that the sustainable cutting technique is highly efficient when applied to fabric with a width of 115 cm to produce five clothing items. The wastra used should have a pattern that can be rotated without considering the position of the motifs that must meet each other.

Greckie wyrazy βόρατον, βράθυ, βουρί jako przykłady zapożyczenia wielokrotnego

The paper discusses three Ancient Greek appellatives βόρατον, βράθυ, βουρί denoting conifers from the Cupressaceae family and demonstrates a common Semitic origin of these dendronyms. They should be treated as examples of multiple borrowing, the ultimate source of which was the uniform Proto-Semitic archetype *burāṯ- ‘juniper, Juniperus L.’. It should be assumed that the ancient Greeks borrowed two synonymous terms βόρατον n. ‘stinking juniper, Juniperus foetidissima Willd.; savin juniper, Juniperus sabina L.’ and βράθυ n. ‘id.’ from two different Aramaic sources. On the other hand, the Pamphylian dialectism βουρί n. ‘Mediterranean cypress, Cupressus sempervirens L.’ was borrowed from an Akkadian source via Anatolian languages to Ancient Greek (Gk. Pamph. βουρί n. ‘cypress’ ← Lycian *burhi < *burehi < Luwian *burašiš c. ← Assyrian or Akkadian burāšu ‘(Phoenician) juniper’ < Old Akkadian burāšum ‘juniper’ < Proto-Semitic *burāṯ-). A carefully conducted analysis of lexical data clearly demonstrates that language contacts between the Semites and the Greeks took place at different times and in many places, so potential Semitisms could have gradually penetrated the Greek vocabulary by various ways.

The geochronometry of Idaho and the bumpy barcode revisited: Snake River detrital zircons in Hells Canyon and beyond

Detrital zircons in modern stream sands and terraces of the Snake River drainage upstream of and within Hells Canyon, western Idaho, U.S.A, effectively reproduce the geochronometry of Idaho magmatic rocks, both from Laurentia in eastern Idaho, and from the accreted terranes west of the Salmon River Suture. We used large-n (300 grain) analysis of detrital zircon ages and Monte Carlo-based mixture modeling to estimate the percent contributions from the upper Snake River and several tributaries. The large number of grains analyzed allows more precise statistical modeling than previous studies, which used 60 or 100 grains.Immediately upstream of the Hells Canyon Complex of dams modeling suggests that the Snake River at Farewell Bend contains detrital zircon contributions of Payette River 50 % and Boise River 10 % (mainly from the Atlanta lobe, Idaho batholith). The upper Snake River has 30 % contribution and contains a complex detrital zircon signature including both primary zircons derived from magmatic sources and recycled zircons derived from sedimentary rocks with an ultimate magmatic source. Thus, 60 % of the detrital zircons come from the 98–73 Ma southern Idaho batholith, with less than a third coming from the upper Snake River drainage, despite it representing 60 % of the drainage area. The Owyhee, Malheur, and Weiser rivers contribute <5 % each.Within Hells Canyon, modeling suggests that the main Snake River contributes by far the largest component (85 %); side canyons contribute <5 % of the zircon load. Mixing models for Snake River stream sediment downstream of Lewiston, below Lower Granite Dam (sampled from sands deposited before installation of the dam), suggest 53 % contribution from the main Snake River above the Salmon River, 34 % from the Clearwater River, 7 % from the Salmon River, and 6 % from the Grande Ronde River.Comparing relative zircon inputs from the modern Snake and Salmon rivers to a pre-dam river terrace just downstream from their confluence suggests that the Snake River in Hells Canyon today contributes only 4 % of the detrital zircons whereas before installation of the Hells Canyon Dams it contributed 29 %. We interpret this reduction in detrital zircon supply to be caused by sediment trapping above the dams.One influence on the detrital zircon contribution of various streams is peak flow volume. Zircon fertility of specific source rocks is the main influence on detrital zircon percentages within individual drainages. Mesoproterozoic, Cretaceous and Eocene granitic rocks produce euhedral magmatic detrital zircon grains that dominate several drainages. Mesozoic metavolcanic and Eocene Challis Volcanic Group rocks yield fewer and often broken detrital zircon grains. Large outcrop areas of Neogene Columbia River and Snake River Plain basalts provide almost none. Recycling of older magmatic detrital zircon through Proterozoic and Paleozoic sandstones is a signature of the eastern and central Idaho thrust belt.