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Meanwhile, streamlines between the same injector and producer can be subdivided to describe driving capacity distribution in water phase, providing useful information for the decision making of water flooding optimization, well pattern adjustment and deep profile modification.
Fig. 7 Differences in a 500 hPa and b 850 hPa streamlines between high EASMI years and low EASMI years.
The results of analysis of differences in 850 hPa streamlines between the two groups also show similar spatial distributions to those shown by the results of analysis of differences in 500 hPa streamlines (Fig. 7b).
With regard to differences in 850 and 500 hPa streamlines between the two groups, anomalous cyclones were reinforced in the western North Pacific and anomalous anticyclones were reinforced in the mid-latitudes of East Asia in high EASMI years.
Based on the difference in 500 hPa streamlines between the two variables, it can be seen that while anomalous cyclonic circulations were reinforced in the western North Pacific, anomalous anticyclonic circulations were reinforced in mid-latitudes in the analysis area (Fig. 7a).
Furthermore, we recorded the number of streamlines between thalamus and lobar target as a proportion of the number going to all target areas.
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Soil samples were taken along a streamline between the recharge canal and the first monitoring well.
The comparison shows a distinct difference of the predicted wetness fraction distribution along the streamline between the equilibrium model and the non-equilibrium model.
During the following steam flooding process, the injected steam will invade along with the main streamline between the injector and the producer.
So in order to obtain the heat intrusion radius, the heat intrusion temperature and the temperature distribution on the main streamline between the injector and the incomplete breakthrough producer should be firstly obtained.
The dark areas in the figures can approximately symbolize the water flooded area or steam and condensate water area and the red curves reveal the difference of the streamline between water flooding and steam flooding when the water or the steam advances into the producer.
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