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Study on Measurement and Influencing Factorsof Trade Embodied Carbon-Based on China-RussiaAgricultural Products Trade 基于中俄农产品贸易的贸易体现碳测量及影响因素研究
Pub Date : 2024-04-25 DOI: 10.15244/pjoes/183075
Wei Wei, Qiyuan Li, Zichao Yu, Yunzhe Wang, Hao Wang
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引用次数: 0
Studying Optimal Strategies of TransmissionCongestion Management in the Spot Market 研究现货市场输电拥塞管理的最佳策略
Pub Date : 2024-04-25 DOI: 10.15244/pjoes/173993
Xiaodong Chen, Su Yang, Longxia Ren, Xingen Wang
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引用次数: 0
An Identification Method of Maize Crop’sNutritional Status Based on Index Weight 基于指数重量的玉米作物营养状况鉴定方法
Pub Date : 2024-04-25 DOI: 10.15244/pjoes/176066
Li Tian, Chun Wang, Hailiang Li, Haitian Sun
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引用次数: 0
Neuropharmacological Evaluation and AntioxidantPotential of Aloe Barbadensis, Capparis Spinosaand Senegalia Senegal Extract in Mice 芦荟、刺槐和塞内加尔提取物在小鼠中的神经药理学评价和抗氧化潜力
Pub Date : 2024-04-25 DOI: 10.15244/pjoes/177428
S. Alnasser
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引用次数: 0
Soil Cations Explain the Variation of SoilExtracellular Activities and Microbial ElementalLimitations on Subtropical Grassland, China 土壤阳离子解释中国亚热带草原土壤胞外活性和微生物元素限制的变化
Pub Date : 2024-04-24 DOI: 10.15244/pjoes/176566
Leilei Ding, Hong Chen, Xin Wei, Taoying Qin, Xia Lei, Jingyi Li, Yujun Zhang, Lili Zhao, Puchang Wang
The objective of this study was to compare the effects of grazing and non-grazing on the physicochemical properties, stoichiometry, ecto-enzyme activities, and microbial element limitations of soils at five depths in subtropical grassland, China, and to identify the influencing factors of enzyme activities and element limitations. Results showed that grazing, soil depth, and the interaction between grazing and depth remarkably changed soil available phosphorus (AP), available potassium (AK), available calcium (ACa) and available magnesium contents (AMg), bulk density (BD), water content (WC), and β-glucosidase activity (βGC) ( p = 6.702e-9 - 0.04739). Compared with no grazing, grazing remarkably declined the 0-5 cm soil AP by 73.10% ( p = 0.0250), the 0-5, 5-10, 10-20 cm soil WC by 47.19% ( p = 0.0042), 37.19% ( p = 0.0090), and 30.80% ( p = 0.0034), however, grazing remarkably increased the 0-5, 5-10, 10-20, 20-30 cm soil ACa by 188.76% ( p = 7.9e-05), 93.24% ( p = 0.0177) ,84.18% ( p = 0.00067), and 38.77% ( p = 0.01368), the 0-5, 5-10 cm soil AMg by 186.69% ( p = 0.0016), 78.89% ( p = 0.0109), the 0-5, 5-10, 10-20 cm soil pH by 0.51 ( p = 0.0013), 0.37 ( p = 0.0006), and 0.27 ( p = 0.0114) units, the 0-5, 5-10, 10-20 cm soil BD by 59.03% ( p = 0.0077), 44.14% ( p = 0.0147), and 35.55% ( p = 0.0071), the 30-50 cm soil WC by 22.88% ( p = 0.0241), the 0-5 cm soil βGC by 89.49% ( p = 0.0011), the 0-5, 5-10 cm soil ACP by 7.87% ( p = 0.0300), 6.57% ( p = 0.0240), respectively. Grazing exacerbated the microbial C limitation of 0-5 and 10-20 cm soils by 20.51% ( p = 0.0078) and 40.38% ( p = 0.0209) and switched the soil microbiome from under N limitation to under P limitation at 5-10 cm ( p = 0.0390). Specific soil available cations were identified as the important factors that significantly explained the variation of soil ecto-enzyme activities and soil microbial carbon and nutrient limitations.
本研究旨在比较放牧和非放牧对中国亚热带草原5个深度土壤理化性质、化学计量学、外源酶活性和微生物元素限制的影响,并确定酶活性和元素限制的影响因素。结果表明,放牧、土壤深度以及放牧与土壤深度的交互作用显著改变了土壤可利用磷(AP)、可利用钾(AK)、可利用钙(ACa)和可利用镁(AMg)含量、容重(BD)、含水量(WC)和β-葡萄糖苷酶活性(βGC)(p = 6.702e-9 - 0.04739)。与不放牧相比,放牧显著降低了 0-5 厘米土壤 AP 的 73.10%( p = 0.0250),0-5、5-10、10-20 厘米土壤 WC 的 47.19%( p = 0.0042)、37.19%( p = 0.0090)和 30.80%( p = 0.0034),但放牧显著增加了 0-5、5-10、10-20、20-30 cm 土壤 ACa 188.76%( p = 7.9e-05) 、93.24%( p = 0.0177) 、84.18%( p = 0.00067) 和 38.77%( p = 0.01368),0-5、5-10 cm 土壤 AMg 186.69%( p = 0.0016)、78.89%(p = 0.0109),0-5、5-10、10-20 cm 土壤 pH 值分别降低 0.51(p = 0.0013)、0.37(p = 0.0006)、0.27(p = 0.0114)个单位,0-5、5-10、10-20 cm 土壤 BD 值分别降低 59.03%(p = 0.0077)、44.14%(p = 0.0147) 和 35.55% ( p = 0.0071),30-50 cm 土壤 WC 分别降低 22.88% ( p = 0.0241),0-5 cm 土壤 βGC 降低 89.49% ( p = 0.0011),0-5、5-10 cm 土壤 ACP 分别降低 7.87% ( p = 0.0300)、6.57% ( p = 0.0240)。放牧加剧了 0-5 和 10-20 厘米土壤微生物的 C 限制,分别为 20.51% ( p = 0.0078) 和 40.38% ( p = 0.0209),并使 5-10 厘米土壤微生物群从 N 限制转为 P 限制 ( p = 0.0390)。特定的土壤可利用阳离子被认为是显著解释土壤外切酶活性和土壤微生物碳和养分限制变化的重要因素。
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引用次数: 0
Hydrochemical Characteristics and ReverseHydrogeochemical Modeling of TaiyuanFormation Limestone Groundwater ofSunan Mining Area in Huaibei Coalfield 淮北煤田苏南矿区太原造山运动石灰岩地下水的水化学特征及反演水地球化学模型
Pub Date : 2024-04-24 DOI: 10.15244/pjoes/176555
Wei Gong, Wei Hua Peng, Zhi Chun Li, Jie Ma, Hao Yu, Pan Xu, Jiajie Zhang
Taiyuan Formation limestone groundwater is the main aquifer threatening the safety of exploration under deep mining in the Huaibei coalfield. Therefore, acknowledging the hydrochemical characteristics and constructing reverse hydrogeochemical modeling are crucial for predicting and preventing mine water hazards. In this study, the mathematical statistical analysis, Piper three-line diagram, Gibbs diagram, ion proportional relationship, Chlorine-Alkali index, and the reverse hydrogeochemical modeling were employed for determining the hydrochemical characteristics and the formation mechanism. The results revealed that the hydrochemical types of groundwater samples were SO 4 .Cl-Ca.Mg and HCO 3 .Cl-Na, respectively. The water-rock interactions were primarily influenced by the leaching and the cation exchange, with these processes being more intense in the eastern region. Through reverse hydrogeochemical modeling, the water-rock interactions in the process of groundwater runoff were quantitatively verified, viz. the calcite and the dolomite were saturated and precipitating, while the gypsum and the halite were unsaturated and still dissolving. Furthermore, the simulations of mass transfer in groundwater runoff indicated that the dissolution and the leaching of gypsum, dolomite and halite, positive ion exchange, the precipitation of calcite, and the dissolution of CO 2 gas predominantly occurred along four simulated flow paths. These results offered a scientific foundation for the prevention and controlling of mine water hazards in deep mining contexts.
太原地层石灰岩地下水是威胁淮北煤田深部开采安全的主要含水层。因此,认识其水文地质化学特征,建立反演水文地质化学模型是预测和预防矿井水危害的关键。本研究采用数理统计分析、Piper 三线图、Gibbs 图、离子比例关系、氯碱指数和逆向水文地质化学模型来确定水化学特征和形成机理。结果表明,地下水样本的水化学类型分别为 SO 4 .Cl-Ca.Mg和HCO 3 .Cl-Na。水与岩石之间的相互作用主要受浸滤作用和阳离子交换作用的影响,其中东部地区的浸滤作用和阳离子交换作用更为强烈。通过反演水文地球化学模型,定量验证了地下水径流过程中的水岩相互作用,即方解石和白云石处于饱和沉淀状态,而石膏和海泡石处于非饱和溶解状态。此外,地下水径流的传质模拟表明,石膏、白云石和卤石的溶解和浸出、正离子交换、方解石的沉淀以及二氧化碳气体的溶解主要发生在四条模拟流路上。这些结果为预防和控制深部采矿环境中的矿井水危害提供了科学依据。
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引用次数: 0
Strong Provincial Capital Strategy and the Qualityof Regional Green and Low-Carbon Development– Empirical Analysis Based on the Expansionof Provincial Capital City Boundaries 强省会战略与区域绿色低碳发展质量--基于省会城市边界拓展的实证分析
Pub Date : 2024-04-24 DOI: 10.15244/pjoes/177431
Rongbo Zhang, Changbiao Zhong
Based on literature review and theoretical mechanisms, this article selects city-level data to explore the impact of provincial capital cities boundary expansion on the quality of regional green and low-carbon development. The following conclusions were obtained: (1) Overall, the expansion of provincial capital city boundaries can significantly improve the quality of green and low-carbon development in the later stages of policy implementation, which in turn significantly improves the benefits of urban green and low-carbon development. The estimated coefficients of policy effects show a trend of slow increase followed by a significant increase. (2) The analysis of Hefei City as a case sample discovered, that expansion of the provincial capital city boundaries can bring about the policy effect of about 0.002-0.371 units to Hefei. From the perspective of the development trend, in the early stage of policy implementation (2011-2014), the degree of policy effect enhancement is slow, and the positive green low-carbon effect has not been fully utilized. In the middle and late stages of policy implementation (2015-2019), the green low-carbon effect shows an increasing development. The policy effect coefficient peaked in 2016, with a value of 0.371. (3) After the implementation of the “strong provincial capital” strategy, the efficient utilization of infrastructure construction, the reduction of industrial transfer, the positive externalities of industrial agglomeration, and the expansion of the city’s financial autonomy are the mechanism paths that generate positive green and low-carbon effects in the later stages of policy implementation.
本文在文献综述和理论机理的基础上,选取城市层面的数据,探讨省会城市边界扩张对区域绿色低碳发展质量的影响。得出以下结论:(1)总体而言,省会城市边界扩张能够在政策实施后期显著提高绿色低碳发展质量,进而显著提高城市绿色低碳发展效益。政策效应的估计系数呈现先缓慢上升后显著上升的趋势。(2)以合肥市为案例样本分析发现,省会城市边界的扩大可为合肥带来约 0.002-0.371 个单位的政策效应。从发展趋势来看,在政策实施初期(2011-2014 年),政策效应提升程度较慢,绿色低碳正效应尚未充分发挥。在政策实施的中后期(2015-2019 年),绿色低碳效应呈现出不断增强的发展态势。政策效应系数在 2016 年达到峰值,数值为 0.371。(3)"强省会 "战略实施后,基础设施建设的高效利用、产业转移的减少、产业集聚的正外部性、城市财政自主权的扩大是政策实施后期产生绿色低碳正效应的机制路径。
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引用次数: 0
Comparative Analysis of Soil Salinity under Flatand Ridge Cultivation Methods in Citrus Orchards 柑橘园平地和山脊栽培法下的土壤盐度对比分析
Pub Date : 2024-04-24 DOI: 10.15244/pjoes/184629
Burçak Kapur
quantify
量化
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引用次数: 0
Occurrence of Single and Mixed Viral Infectionsof Grapevine (Vitis Spp.) in Azerbaijan 阿塞拜疆葡萄(葡萄属)单一和混合病毒感染的发生情况
Pub Date : 2024-04-24 DOI: 10.15244/pjoes/176052
Nargiz Sultanova, Mina Rastgou, I. Huseynova
Viruses can adversely affect vines' vitality, longevity, quality, and quantity in single or mixed infections. In this work, to detect single and mixed viral infections of grapevine in two central viticulture regions of Azerbaijan, a total of 166 samples showing virus-like symptoms including yellows, reddening, fan leaf, mosaic, leaf rolling, and shortening of internodes were collected during the growing seasons of 2022-2023 from different vineyards and subjected to ELISA and RT-PCR analyses. Plant samples were initially assayed using the one-step assay AgriStrip based on lateral flow immunochromatography and DAS-ELISA with specific antisera for Grapevine fanleaf virus (GFLV), Grapevine leafroll-associated virus 1 (GLRaV-1), Grapevine leafroll-associated virus 2 (GLRaV-2), Grapevine leafroll-associated virus 3 (GLRaV-3), and Grapevine leafroll-associated virus 4 (GLRaV-4). Following serological tests, 65% (108 out of 166) of the examined samples exhibited a positive result for one or more of the specified viruses. Total RNA was extracted, and synthesized cDNA was used to amplify a part of the coat protein (CP) gene in RT-PCR using specific primers. Amplicons of the expected size of 1560 bp, 401 bp, 600 bp, 942 bp, 500 bp, and 272 bp were amplified for the mentioned viruses, respectively (but not from healthy samples). The result of this study can be used in the management strategies of these viruses in grapevine-producing areas of Azerbaijan.
病毒在单一或混合感染的情况下会对葡萄树的生命力、寿命、质量和数量产生不利影响。在这项工作中,为了检测阿塞拜疆两个中部葡萄栽培区葡萄藤的单一和混合病毒感染情况,我们在 2022-2023 年的生长季节从不同的葡萄园收集了 166 个出现病毒样症状的样本,包括黄化、变红、扇形叶、镶嵌、卷叶和节间缩短,并进行了 ELISA 和 RT-PCR 分析。植物样本最初使用基于侧流免疫层析和 DAS-ELISA 的葡萄扇叶病毒(GFLV)特异性抗血清一步法检测 AgriStrip、葡萄花叶病毒 1 (GLRaV-1)、葡萄花叶病毒 2 (GLRaV-2)、葡萄花叶病毒 3 (GLRaV-3) 和葡萄花叶病毒 4 (GLRaV-4)。经过血清学检测,65%的受检样本(166 份样本中有 108 份)对一种或多种指定病毒呈阳性结果。提取总 RNA,合成 cDNA,使用特异引物在 RT-PCR 中扩增衣壳蛋白(CP)基因的一部分。结果显示,上述病毒分别扩增出预期大小为 1560 bp、401 bp、600 bp、942 bp、500 bp 和 272 bp 的扩增子(但健康样本中没有)。本研究结果可用于阿塞拜疆葡萄产区对这些病毒的管理策略。
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引用次数: 0
Study on the Effect of Soil Moistureon Soil Organic Carbon During the GrowingPeriod of Plants in the Subalpine MeadowsZone of Qilian Mountains, China 祁连山亚高山草甸植物生长期土壤水分对土壤有机碳的影响研究
Pub Date : 2024-04-24 DOI: 10.15244/pjoes/176063
Xin Lan, Wen-xiong Jia, Le Yang, Guofeng Zhu, Yue Zhang, Zhijie Yu, Huifang Luo
Soil organic carbon (SOC) is an important component of the global carbon pool, whose accumulation and decomposition affect the balance of the global carbon cycle and climate change. However, understanding of the responses of SOC in alpine ecosystems to climate change is quite limited, especially in the seasonal-frozen soil zone. In order to understand the impact of soil moisture changes on the carbon cycle in alpine mountain ecosystems, we established two sample plots of the semi-shady and semi-sunny slopes in the subalpine meadow zone of the eastern part of Qilian Mountains, and collected soil samples to investigate the spatial and temporal changes of SOC and soil moisture and their relationships. The study indicated that the SOC content showed significant surface aggregation during the plant growing season, and that the influence of soil moisture on SOC was different in different slope directions and soil depths. The influence of soil moisture on SOC was greater on the semi-shady slope than on the semi-sunny slope. Among different soil layer depths, the soil moisture most significantly affected SOC in the soil layer of 20-40 cm. This study provides a theoretical basis for the study of carbon stocks and carbon cycling at high altitudes.
土壤有机碳(SOC)是全球碳库的重要组成部分,其积累和分解影响着全球碳循环的平衡和气候变化。然而,人们对高山生态系统中土壤有机碳对气候变化的反应的了解还很有限,尤其是在季节性冰冻土壤区。为了了解土壤水分变化对高寒山区生态系统碳循环的影响,我们在祁连山东部亚高山草甸带半阴坡和半阳坡建立了两个样地,采集了土壤样品,研究了SOC和土壤水分的时空变化及其关系。研究表明,在植物生长季节,SOC含量呈现出明显的表面聚集现象,不同坡向和土层深度的土壤水分对SOC的影响不同。半阴坡土壤水分对 SOC 的影响大于半阳坡。在不同土层深度中,土壤水分对 20-40 厘米土层的 SOC 影响最大。该研究为研究高海拔地区的碳储量和碳循环提供了理论依据。
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引用次数: 0
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Polish Journal of Environmental Studies
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