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The recognition of named entities in the field of water conservancy is of great significance for the building of water conservancy knowledge graphs and intelligent question answering systems. However, in the current field of water conservancy, there are shortcomings in named entity recognition, such as a lack of annotated corpus, low recognition accuracy of traditional methods and inability to solve polysemous entities. Aiming at the characteristics of water conservancy texts, a Named Entity Recognition Model for Machine Reading Comprehension (MRC) based on data (vocabulary and entity type labels) enhancement, namely the MRC-WLE model was put forward. Mainly, the vocabulary feature information and entity type label feature information in water conservancy texts were injected into the model as "knowledge". It introduced models such as BERT-CRF, BERT-CRF-Word, BERT-BILSTM-CRF and BERT-BILSTM-CRF-Word as controls to evaluate the performance of the MRC-WLE model. The results show that compared with the BERT-CRF and other models mentioned above, the micro average F1 value of the MRC-WLE model has been improved. Compared with the MRC model, the micro average F1 value of the MRC-WLE model has been increased by 0.85%, reflecting the effectiveness of data augmentation. [ABSTRACT FROM AUTHOR]

Copyright of Journal of Anhui Agricultural Sciences is the property of Journal of Anhui Agricultural Sciences Editorial Office 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 order to study the mechanical properties and failure characteristics of layered shale in New Yan'an Tunnel and analyze the influence of different inclination angles of bedding plane on rock mechanical parameters. Laboratory uniaxial compression, triaxial compression and Brazil splitting tests and numerical uniaxial compression and triaxial compression tests under different bedding angles were carried out. The laboratory test analysis show that the peak intensity first decreases and then increases with the increase of inclination angle. The compressive strength shows a U-shaped trend, the elastic modulus changes in a “V” shape. And through a large number of numerical simulation tests to expand the scope of laboratory tests and the relationships between compressive strength and elastic modulus with dip angle were fitted respectively. The increase of confining pressure weakens shale anisotropy, but the degree of weakening decreases with the increasing of confining pressure. The strength of laminated shale is weakened by cohesion much more than internal friction angle. The tensile strength decreases with the increase of inclination angle. The failure modes of layered shale are different with different inclination angles, under the condition of uniaxial compression, tensile failure occurs for 0°, shear slip failure along the bedding plane controlled by the weak plane occurs at 30° ~ 60°, cleavage tensile failure occurs at 90°. Under triaxial compression, the shale specimens with different bedding plane inclinations mainly undergo shear failure. [ABSTRACT FROM AUTHOR]

Copyright of Science Technology & Industry is the property of Chinese Society of Technology Economics 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 Southwest China Journal of Agricultural Sciences is the property of Editorial Department of Southwest China Journal of Agricultural 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 Hydrometallurgy of China is the property of Hydrometallurgy of China Editorial Office 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.)

Soil water deficit is the main obstacle factor of plant reconstruction in rocky desertification area of Southwest China. Mycorrhizal mulberry (Morus alba L.) can cope with the main ecological barriers during the seasonal drought in the rocky desertification area. However, it is unclear the water resource of mulberry. In this study, we studied the water use strategy of mulberry root in different seasons by hydrogen and oxygen stable isotope technique. The mulberry was grown in typical rocky desertification area in Qingshuipu town, Qixingguan district, Bijie city (105°35′02′′E, 27°41′19′′N) in Guizhou Province. The precipitation was mainly concentrated in June-September. The mulberry was not irrigated. The annual growth of mulberry was in 2 seasons: from April to June and from September to November. The samples of rainfall water, soil and plant branch were collected from April to November of 2014. Soil was sampled at 0-60 cm depth with 10 cm as a sampling layer. The abundance of deuterium and oxygen stable isotope were measured. The correction analysis method was used to preliminarily evaluate water sources of mulberry. The contribution rate of water at each soil layer was also calculated. The results showed that in rainfall water, the abundance of deuterium from April to November averaged -25.9‰ and the oxygen stable isotope abundance averaged -4.82‰. In spring from April to June, the abundance of deuterium and oxygen stable isotope in rainfall water averaged -0.24‰ and -1.68‰, respectively. In autumn from September to November, the abundance of deuterium and oxygen stable isotope in rainfall water averaged -60.0‰ and -8.17‰, respectively. In spring, the abundance of deuterium and oxygen stable isotope in soil water averaged -29.4‰ and -4.77‰, respectively while the abundance of deuterium and oxygen stable isotope in xylem water averaged -33.2‰ and -5.39‰, respectively. In autumn, the abundance of deuterium and oxygen stable isotope in soil water averaged -70.1‰ and -9.27‰, respectively while the abundance of deuterium and oxygen stable isotope in xylem water averaged -55.7‰ and -7.92‰, respectively. The abundance of both stable isotopes in soil water and xylem water were below that in the rainfall water and that of xylem water were between soil water and rainfall water. It indicated that the mulberry mainly used soil water. Both isotopes in rainwater were more enriched in the early stage of mulberry growth (spring, from April to June) than in the late growth stages (autumn, from September to November). With the seasonal variation of rainfall, the both isotopes of soil water showed a downward trend. According to rainfall water equations, the mulberry absorbed mainly soil water. Both isotopes had clear seasonal trend. In spring, the isotopes in soil water decreased with the increase of soil depth. In autumn, isotopes in soil water decreased then increased with soil depth. Based on the correlation method, the mulberry absorbed water from different soil depth. In spring, it absorbed water from soil below 20 cm while it absorbed water from soil 0-20 cm. In September, it also absorbed water from 50-60 cm soil layer. Based on results from the IsoSource software, in spring, mulberry mainly used soil water from soil layers of 10-30 to 50-60 cm. In autumn, it mainly used soil water from soil layers of 50-60 to 0-10 cm. In spring, the contribution rate was 69.1% by 10-30 cm in soil, 31.8% and 66% by 50-60 cm layer in May and June, 70.2% by 50-60 cm in September and 94.3% and 71.9% by 0-10 cm in October and November, respectively. The study will be helpful to mulberry manage and application in rocky desertification area. [ABSTRACT FROM AUTHOR]

Copyright of Journal of Agricultural Science & Technology (1008-0864) is the property of Journal of Agricultural 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 Journal of Henan Agricultural Sciences is the property of Editorial Board of Journal of Henan Agricultural 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 Journal of Southern Agriculture is the property of Journal of Southern Agriculture 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.)