Zobrazeno 1 - 10
of 50
pro vyhledávání: '"Guangrong ZHANG"'
Autor:
Wenqiang An, Jianzhao Xu, Fang Chen, Yongcai Ma, Zeliang Su, Junfeng Guang, Ningning Su, Guangrong Zhang, Chao Xu, Yuanyou Li, Dizhi Xie
Publikováno v:
Aquaculture Reports, Vol 32, Iss , Pp 101704- (2023)
The n-3 long chain polyunsaturated fatty acids (n-3 LC-PUFA) play important roles in the normal growth and metabolism of fish . In order to explore the appropriate requiremnts of n-3 LC-PUFA in juvenile largemouth bass Micropterus salmoides, a freshw
Externí odkaz:
https://doaj.org/article/252202476107469e8676cfb77da7a3bd
Autor:
Shuli Yang, Guangrong Zhang, Zaimei Yuan, Shichun He, Rongjiao Wang, Jieyi Zheng, Huaming Mao, Jianmin Chai, Dongwang Wu
Publikováno v:
Frontiers in Veterinary Science, Vol 10 (2023)
The rumen of ruminants is inhabited by complex and diverse microorganisms. Young animals are exposed to a variety of microorganisms from their mother and the environment, and a few colonize and survive in their digestive tracts, forming specific micr
Externí odkaz:
https://doaj.org/article/1f1c0c29e8984ad0830919868caaae96
Publikováno v:
Natural Gas Industry B, Vol 8, Iss 3, Pp 217-230 (2021)
The Wufeng Formation–Longmaxi Formation in the Sichuan Basin in South China is the key stratum for shale gas exploration and production. To date, three national shale gas demonstration zones have been developed. Nevertheless, there are still some t
Externí odkaz:
https://doaj.org/article/b9a57b59b98a473d8311e48379a64b50
Publikováno v:
Natural Gas Industry B, Vol 8, Iss 1, Pp 24-34 (2021)
The Upper Ordovician WufengFm and the Lower Silurian LongmaxiFm are important strata for shale gas exploration and development in the Sichuan Basin, but the genetic mechanism, evolutionary history and the controlling effect of mineral diagenetic evol
Externí odkaz:
https://doaj.org/article/f5d11a81512d4cafb0c90b4399e9c53f
Publikováno v:
Energy Geoscience, Vol 1, Iss 3, Pp 147-164 (2020)
The Fuling shale gas field in China is the largest shale gas field as well as the largest of its type discovered in any Lower Paleozoic formation. In this study, the geology and production of the upper and lower gas layers in the Fuling shale gas fie
Externí odkaz:
https://doaj.org/article/1480da5582eb4cadb90de7ed2fc89df0
Publikováno v:
Shiyou shiyan dizhi, Vol 42, Iss 3, Pp 459-466 (2020)
Pyrite is one of the most common minerals in shale, but its type, genesis and effect on shale gas accumulation are still in the initial study stage. The shale in the Upper Ordovician Wufeng Formation and the Lower Silurian Longmaxi Formation in the S
Externí odkaz:
https://doaj.org/article/9af7a335df884141920879b86bd28047
Publikováno v:
Natural Gas Industry B, Vol 5, Iss 4, Pp 360-370 (2018)
The northern Sichuan Basin, spreading in the northern section of the Longmenshan Fault Fold Belt, is characterized by dramatic fluctuations in the surface landforms, development of abdominal faults, and low-quality seismic data, resulting in difficul
Externí odkaz:
https://doaj.org/article/2b7ab2df37524f628b0fc52a02a442de
Publikováno v:
Natural Gas Industry B, Vol 4, Iss 3, Pp 203-211 (2017)
The Lower Cambrian Longwangmiao Fm gas reservoir in the Gaoshiti–Moxi area, the Sichuan Basin, is a super giant monoblock marine carbonate gas reservoir with its single size being the largest in China. The key to the realization of high and stable
Externí odkaz:
https://doaj.org/article/e4f32dac7463461687fb1b877857685c
Autor:
Guangrong Zhang, Qi Ran, Qi Liao, Yi Yu, Xuan Zhang, Kang Chen, Hong Cao, Ming Zeng, Long Wen, Qiang Lai
Publikováno v:
Natural Gas Industry B, Vol 3, Iss 4, Pp 323-329 (2016)
The dolomite reservoirs of the Lower Cambrian Longwangmiao Fm in the Gaoshiti–Moxi area, Sichuan Basin, are deeply buried (generally 4400–4900 m), with high heterogeneity, making reservoir prediction difficult. In this regard, key seismic explora
Externí odkaz:
https://doaj.org/article/e469f48aeceb4026813750742373602e
Publikováno v:
Advances in Difference Equations, Vol 2010 (2010)
We establish some new oscillation criteria for the second-order quasilinear neutral delay dynamic equations [r(t)(zΔ(t))γ]Δ+q1(t)xα(τ1(t))+q2(t)xβ(τ2(t))=0 on a time scale 𝕋, where z(t)=x(t)+p(t)x(τ0(t)), 0
Externí odkaz:
https://doaj.org/article/181d2d317f214669b5c6257d2a8a3c84