southwestern guizhou
Recently Published Documents


TOTAL DOCUMENTS

53
(FIVE YEARS 15)

H-INDEX

11
(FIVE YEARS 1)

PLoS ONE ◽  
2021 ◽  
Vol 16 (12) ◽  
pp. e0260779
Author(s):  
Xiaoqian Yang ◽  
Youcai Tuo ◽  
Yanjing Yang ◽  
Xin Wang ◽  
Yun Deng ◽  
...  

The front retaining wall (FRW) is an effective facility of selective withdrawal. Previous research has not estimated the effect of FRWs on the thermal regimes of reservoirs and outflow temperature, which are crucial to reservoir ecology. For this purpose, taking the Dongqing Reservoir as a case study, a two-dimensional hydrodynamic CE-QUAL-W2 model was configured for the typical channel-type reservoir in the southwestern Guizhou Province, to better understand the influence of FRWs on the thermal structure and outflow temperature. The simulated data from January to September 2017 showed that FRWs can change the vertical temperature distribution during the stratification period, accelerate the upper warmer water release and thus decrease the strength of thermal stratification. The stratification structure changed from a single thermocline to double thermoclines in August. An FRW resulted in an average 11.8 m increase in the thickness of the hypolimnion and a 1.2°C decrease in the thickness of the thermocline layer. An FRW increased the outflow temperature by 0.4°C and raised the withdrawal elevation by 16 m on average. The longitudinal velocity increased compared with the non-FRW condition, while the maximum velocity position moved up. In addition, FRWs can continuously obtain surface warmer water without manual operation and have low investment and good construction conditions. This study can provide an available selective withdrawal idea for reservoirs with similar hydraulic conditions.


Minerals ◽  
2021 ◽  
Vol 11 (7) ◽  
pp. 737
Author(s):  
Jun Sun ◽  
Yunlong Liu ◽  
Xiqiang Liu

The Shazi deposit is a newly discovered, potential large-scale scandium deposit located in Qinglong, southwestern Guizhou Province, China. The iron isotopic composition of magnetite in fresh basalt, weathered basalt, and mineralized laterite was investigated. The Fe content of fresh basalt and of weathered basalt vary from 15.41 wt.% to 15.51 wt.% and from 14.60 wt.% to 15.12 wt.%, respectively, while the δ56Fe of magnetite varies from 0.23‰ to 0.29‰ and from 0.02‰ to 0.07‰. Laterite has the highest Fe content, in the range of 23.53%~28.95%, but δ56Fe is similar to weathered basalt, and the range of variation is −0.09‰–0.03‰. The change in iron isotope composition in weathered basalt and laterite is related to the hydrolysis of clinopyroxene. Combined with the existing research results, the genesis of scandium deposit is considered to be related to in situ hydrolysis in deep and surface weathering leaching of Emeishan basalt.


2021 ◽  
Vol 9 (1) ◽  
pp. 1199-1212
Author(s):  
Jiliang Huang

Comprehensively improving the quality of education in resource-poor areas is an urgent challenge to achieve balanced development of basic education in China. In the process of educational development in resource-lacking areas, information technology has: (1) changed the traditional teaching mode and teaching environment, (2) provided high-quality educational resources, (3) promoted the professional development of teachers, and (4) promoted the overall improvement of education quality. Southwestern Guizhou Prefecture in Guizhou Province, China, has become a typical case in using information technology to promote education quality improvement in areas with scarce educational resources. This article explores educational information technology in the region as an example to discuss how to grasp the regional characteristics and local needs in the layout of information technology, integrate information technology into teaching practice, and steadily improve the overall teaching quality of the region.


Zootaxa ◽  
2021 ◽  
Vol 4985 (2) ◽  
Author(s):  
MINGYI TIAN ◽  
SUNBIN HUANG

Ckacus youcha n. gen. & n. sp. is described and illustrated based on a single male discovered in the deep area of Luoshui Dong, a vertical cave in Anlong Xian, southwestern most of Guizhou Province, Southwest China. This new genus seems related to Bathytrechus Uéno, 2005 from Leye Xian, northwestern most Guangxi by its elongate body which is wholly pubescent, the tridentate right mandible and the well-striated elytra with the 1st interval extremely narrowed at apical 1/3, but differs in several important characters. In addition, three individuals of the species Satotrechus rieae Uéno, 2006 were also collected from -340 m to -450 m in the same cave. This species was formerly only known from four caves in Anlong and Ceheng counties.


Minerals ◽  
2021 ◽  
Vol 11 (2) ◽  
pp. 100
Author(s):  
Zepeng Wang ◽  
Qinping Tan ◽  
Yong Xia ◽  
Jianzhong Liu ◽  
Chengfu Yang ◽  
...  

Southwestern Guizhou, China, is famous for hosting clusters of Carlin-type Au, Sb, and Hg-Tl deposits. These deposits are thought to be the products of a low-temperature hydrothermal metallogenic event. Calcite and fluorite are common and widespread gangue minerals in Au and Sb deposits, respectively. Ore-related calcite commonly coexists with stibnite, realgar, and orpiment at the periphery of high-grade orebodies in Au deposits, while ore-related fluorite is generally intergrown with stibnite in Sb deposits. In this study, ore-related calcite and fluorite samples from representative Au (Zimudang) and Sb (Dachang) deposits, respectively, were separated, and the rare earth element (REE) concentrations, Sm/Nd isotope ratios, and Sm–Nd isochron ages were analyzed. This study aims to determine the formation ages of the calcite and fluorite and to constrain the age of low-temperature metallogenic event in Southwestern Guizhou. The calcite and fluorite samples contain relatively high total concentrations of REEs (8.21–22.5 μg/g for calcite, 21.7–36.6 μg/g for fluorite), exhibit variable Sm/Nd ratios (0.51–1.01 for calcite, 0.35–0.49 for fluorite), and yield Sm–Nd isochron ages of 148.4 ± 4.8 and 141 ± 20 Ma, respectively. These ages are consistent with the age range constrained by the low-temperature thermochronology of zircon (132–160 Ma), crosscutting relationships of stratigraphy or intrusions (96–160 Ma), and previous dating results (135–150 Ma) in Southwestern Guizhou. Collectively, the ages obtained in this study add new evidence to previous geochronology studies, such that the low-temperature hydrothermal mineralization in Southwestern Guizhou can be constrained to 135–150 Ma, corresponding to the Yanshanian orogeny, which was associated with a weak extensional tectonic environment.


PhytoKeys ◽  
2020 ◽  
Vol 166 ◽  
pp. 79-86
Author(s):  
Zhi Li ◽  
Hai-Lei Zheng ◽  
Ming Tang

A new species of Asteraceae, Synotis panzhouensis, is described and illustrated from Guizhou Province in China. Compared with other species of the genus, it is distinguishable by having red-purple pappus; additionally, it differs from its closest ally S. nayongensis by the larger involucres and phyllaries, and higher number of phyllaries and disk florets. In addition, detailed discussion of morphological differences, the provisional IUCN status and a distribution map are provided.


Sign in / Sign up

Export Citation Format

Share Document