Analysis on the Factors Affecting the Change of the Ebinur Lake Area

2010 ◽  
Vol 27 (1) ◽  
pp. 64-68 ◽  
Author(s):  
Wen-jun LIU ◽  
Peng ZHANG ◽  
Li-hua LI ◽  
Zhi-min FENG
2015 ◽  
Vol 48 (8) ◽  
pp. 871-880 ◽  
Author(s):  
L. Qin ◽  
G. H. Lv ◽  
X. M. He ◽  
J. J. Yang ◽  
H. L. Wang ◽  
...  

2013 ◽  
Vol 33 (22) ◽  
pp. 7259-7269
Author(s):  
秦璐 QIN Lu ◽  
吕光辉 Lü Guanghui ◽  
何学敏 HE Xuemin ◽  
张雪妮 ZHANG Xueni ◽  
张雪梅 ZHANG Xuemei ◽  
...  

Author(s):  
Ting Chen ◽  
Wenge Hu ◽  
Shuaibing He ◽  
Xue Zhang ◽  
Yanhui Niu

The aim of this study was to reveal the differences in the community structure of AOA between rhizosphere and non-rhizosphere soil, to provide a theoretical basis for further study on the relationship between halophyte rhizosphere soil microorganisms and salt tolerance. The results of diversity and community structure showed that the diversity of ammonia-oxidizing archaea community in rhizosphere soil of Reed was higher than that in non-rhizosphere soil in spring and lower than that in non-rhizosphere soil in summer and autumn; In summer, the diversity of rhizosphere soil was higher than that of non-rhizosphere soil of Karelinia caspica lower than that of non-rhizosphere soil in spring and autumn. The diversity of rhizosphere soil of Halocnemum strobilaceum in three seasons was lower than that in non-rhizosphere soil. The diversity of rhizosphere soil of Salicornia was higher than that in non-rhizosphere soil in three seasons. In addition, the relative abundance of AOA in rhizosphere soil of four plants was higher than that in non-rhizosphere soil. AOA community in all soil samples was mainly concentrated in Crenarchaeota and Thaumarchaeota. RDA results showed salinity (EC), soil water moisture (SM), pH and soil organic matter (SOM) were important factors affecting the differentiation of AOA communities.


1987 ◽  
Vol 44 (S2) ◽  
pp. s239-s248 ◽  
Author(s):  
C. I. Goddard ◽  
D. H. Loftus ◽  
J. A. MacLean ◽  
C. H. Olver ◽  
B. J. Shuter

Creel and lake survey data from 87 Ontario lakes with self-sustaining lake trout (Salvelinus namaycush) populations were analysed to determine the effect of intrinsic factors, such as fish community structure, and extrinsic factors, such as angling-effort, on the observed yields of lake trout. Multiple regression analyses showed that angling-effort and lake area, in order of importance, explained almost 82% of the variation in annual catches. Analyses of covariance were used to test a variety of hypotheses about how community structure — the presence of forage, competitors, or alternate sports species — affected the catch of lake trout. No significant differences among groups were detected, which suggests that fish community structure has little or no effect on actual yield of lake trout. The difficulties inherent in using catch and effort data alone to evaluate the importance of factors affecting productivity (or potential yield) are discussed.


Author(s):  
Tuvshin G ◽  
Khosbayar Ts ◽  
Davaadorj D

This study based on remote sensing methods of changes in the multi-year and seasonal changes in areas of the Buuntsagaan, Orog, Olgoy Lakes in the depression of lakes. Using Landsat 5 and 8 satellite 2000-2017, We used 14 pictures of water and vegetation index those were taken from the lake. Over the past decades, the Gobi region’s lakes have been decreased significantly. There are number of factors affecting changes in areas of the lakes. Finally, we concluded that the water level in the Baidrag and Tuin rivers are decreasing in Buuntsagaan and Orog Lakes.


1977 ◽  
Vol 14 (8) ◽  
pp. 1740-1752
Author(s):  
Hewitt H. Bostock

The compositions of seven pairs of coexisting hornblende and grunerite and five assemblages of coexisting hornblende, grunerite, and garnet from Archean silicate iron formation of low and medium metamorphic grade have been obtained by electron microprobe analysis. Important factors affecting the composition of the amphiboles are: (1) the Mg/Fe ratio of the iron-formation beds, which controls the gross Mg/Fe ratio of the amphiboles; (2) the alumina content of the beds, which affects the degree of alumina substitution in hornblende thereby altering the distribution of Mg and Fe in the coexisting amphiboles; and (3) the occurrence of iron-rich garnet, which produces higher Mg/Fe ratios in both amphiboles. A fourth potentially important factor, the oxygen fugacity, cannot be satisfactorily assessed with these data, but has not obscured the effects of the other three. Temperature of crystallization of the amphiboles was an important factor mainly insofar as it affected the crystallization of garnet in the alumina-rich rocks.Four coexisting hornblende–cummingtonite pairs from metatuffs show similar control of Mg–Fe fractionation by alumina substitution in hornblende.


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