The Effects of Mechanical Degradation and Viscoelastic Behavior on Injectivity of Polyacrylamide Solutions

1983 ◽  
Vol 23 (03) ◽  
pp. 475-485 ◽  
Author(s):  
R.S. Seright

Abstract Results of recent experiments that clarify the effects of mechanical degradation and viscoelastic behavior on the flow of partially hydrolyzed polyacrylamide solutions through porous media are presented. From these results, a simple model that may be used to predict injectivity of polyacrylamide solutions is developed. Injection pressures for linear core floods are shown to be separable into two components:an initial pressure drop associated with the entrance of polymer into the sandstone anda constant pressure gradient throughout the remainder of the core. Entrance pressure throughout the remainder of the core. Entrance pressure drop is zero until the polymer solution flux increases to the rate where mechanical degradation takes place. Thereafter, entrance pressure drop and the degree of polymer mechanical degradation increase with increasing flux. In addition, polymer solutions that undergo a large entrance pressure drop and a high degree of mechanical degradation when first injected into a core show no entrance pressure drop and no further degradation after reinjection into the same core at the same flux. These observations suggest that the entrance pressure drop is associated closely with the process of polymer mechanical degradation. A new correlation is developed that may be used to determine entrance pressure drop and the level of mechanical degradation directly as a function of sand face flux, permeability, and porosity. This correlation is more convenient to apply and less dependent on flow geometry than previous correlations. Based on these observations, a model is developed that may be used to estimate injectivity of polyacrylamide solutions in linear or radial flow geometries. This model takes into account the entrance pressure drop and the dilatant nature of the polymer near the wellbore. Predictions made with this model are compared with experimental results. Introduction This paper reports an investigation of the influence of mechanical degradation and viscoelasticity on the injectivity of partially hydrolyzed polyacrylamide solutions. The viscoelastic nature of the polymer is important primarily at high fluxes that occur near a wellbore. However, mechanical degradation affects the mobility of a polymer bank at all positions within a reservoir. The approach in this report is first to re-examine the process of predicting polymer mechanical degradation in porous media and to simplify the prediction process so that is may more readily be applied to field situations. Next, results of recent experiments that clarify the effects of mechanical degradation and viscoelastic behavior on the flow of polyacrylamide solutions through porous media are presented. Finally, these results are used to develop a simple model to estimate injectivity impairment during a polymer flood. Mechanical Degradation Mechanical degradation means that fluid stresses become large enough to fragment polymer molecules, resulting in an irreversible loss of viscosity and resistance factor. This may happen a porous medium or through a constriction. Resistance factor is defined as the ratio of brine mobility to the mobility of a polymer solution. It may be thought of as the apparent relative viscosity of a polymer solution in porous media. Resistance factors of polyacrylamide solutions are often greater than viscosities. This suggests that polyacrylamides reduce water mobility both by increasing solution viscosity and by reducing effective permeability to water.1,2 Part of the permeability reduction is retained after a polyacrylamide bank is displaced by brine.

2013 ◽  
Vol 807-809 ◽  
pp. 2523-2528
Author(s):  
Yu Fei Jia ◽  
Miao Xu ◽  
Xiao Xiao Liu

Polyacrylamide (polymer) solution which has different relative molecular mass and mass concentration in porous media has been studied in seepage flow experiment. Due to differences in pressure drop at different seepage velocities, the effective viscosities of different polymer solutions are calculated. Rheological behaviors of polymer solution changes in different mass concentration and relative molecular mass in porous media are analyzed. It is indicated that in the range of Darcy seepage velocity, acceleration is increasing during the process of pressure drop on both sides of core is resulted from the increase of flow rate during percolation, its effective viscosity first decreased, then increased with the increases of shear rate at range of Darcy velocity. Higher the relative molecular mass and mass concentration lead greater the effective viscosity.


SPE Journal ◽  
2014 ◽  
Vol 19 (03) ◽  
pp. 373-380 ◽  
Author(s):  
Guoyin Zhang ◽  
R.S.. S. Seright

Summary This paper investigates the effect of hydrolyzed polyacrylamide (HPAM) polymer concentration on retention in porous media by use of both static and dynamic measurements. Consistent results by use of these two methods show that different polymer-retention behaviors exist in dilute, semidilute, and concentrated regions. In both the dilute and concentrated regions, polymer retention has little dependence on concentration. In contrast, in the semidilute region, polymer retention is concentration dependent. If a porous medium is first contacted sufficiently with dilute polymer solution to satisfy the retention, no significant additional retention occurs during exposure to higher HPAM concentrations. On the basis of the experimental results, a concentration-related retention mechanism is proposed that considers the orientation of the adsorbed polymer molecules and the interaction between molecular coils in solution. By use of this model, we explain why polymer retention does not show much dependence on concentration in the dilute and concentrated regimes. Further, in the semidilute region, we explain how moderate coil interactions lead to mixed adsorbed-polymer orientation and magnitude on rock surfaces, and retention becomes concentration dependent. In field applications of polymer and chemical floods, reduced polymer retention may be achieved by first injecting a low-concentration polymer bank.


SPE Journal ◽  
2010 ◽  
Vol 16 (01) ◽  
pp. 35-42 ◽  
Author(s):  
R.S.. S. Seright ◽  
Tianguang Fan ◽  
Kathryn Wavrik ◽  
Rosangela de Carvalho Balaban

Summary This paper clarifies the rheology of xanthan and partially hydrolyzed polyacrylamide (HPAM) solutions in porous media, especially at low velocities. Previous literature reported resistance factors (effective viscosities in porous media) and an apparent shear thinning at low fluxes that were noticeably greater than what is expected on the basis of viscosity measurements. The polymer component that causes the latter behavior is shown to propagate quite slowly and generally will not penetrate deep into a formation. Particularly for HPAM solutions, this behavior can be reduced or eliminated for solutions that experience mechanical degradation or flow through a few feet of porous rock. Under practical conditions where HPAM is used for enhanced oil recovery (EOR), the degree of shear thinning is slight or nonexistent, especially compared to the level of shear thickening that occurs at high fluxes.


1976 ◽  
Vol 16 (04) ◽  
pp. 172-174 ◽  
Author(s):  
J.M. Maerker

Introduction A number of recent papers have addressed the problem of mechanical degradation during injection problem of mechanical degradation during injection into oil reservoirs for secondary or tertiary recovery applications. Ref. 6 introduces and tests a mechanism for mechanical degradation of partially hydrolyzed polyacrylamide solutions and develops a procedure for predicting loss of mobility control in practical situations. The correlation of experimental degradation data on which this procedure depends is based on results of flow procedure depends is based on results of flow through consolidated sandstones only. Porosity was not a variable. Since many applications involve unconsolidated reservoirs, this paper investigates the effects of porosity, permeability, length, and flow rate on mechanical degradation of partially hydrolyzed polyacrylamide solutions in unconsolidated sand packs. A new correlation fitting both types of porous media is developed. The aforementioned correlation (Fig. 4 of Ref. 6) for screen-factor loss in saline polyacrylamide solutions depended on porosity through the correlating group, epsilonLD 1/3. However, the generality of the correlation with regard to porosity dependence was untested, since all the media used to induce degradation (mostly Berea outcrop sandstone) had a porosity of about 24 percent. Subsequent porosity of about 24 percent. Subsequent investigations have been conducted in sand packs with 600-ppm polyacrylamide concentrations in 3.0-percent NaCl plus 0.3-percent CaCl2 to test the porosity dependence and provide more realistic mechanicaldegradation data for application to unconsolidated reservoirs. EXPERIMENTAL PROCEDURE The polymer used was from the same commercially available stock used in Ref. 6, having an estimated average molecular weight between 5 and 7 million and a 20-percent degree of hydrolysis. Sand was packed by sifting into a brine-filled lucite cell designed to eliminate effects of possible degradation caused by a plastic retaining screen at the outlet face. Sand-grain density was assumed to be 2.65 gm/cc, and porosities were determined from weight/volume measurements of sand packed in a brine-filled graduated cylinder. Various sand-grain size fractions were obtained by dry-sieve separation on three different sand sources. The sand packs are described in Table 1. Notice that Sand Packs 1, 3, and 4 were obtained from narrow size ranges, while Sand Pack 5 was a deliberate, broad distribution. RESULTS Experimental screen-factor and viscosity losses induced by flow through the sand packs are analogous to those in Ref. 6 for consolidated sandstones; however, the curves are shifted to larger fluxes (volumetric flow rate divided by cylindrical cross-sectional area) because of higher permeabilities. Plotting screen-factor losses as a permeabilities. Plotting screen-factor losses as a function of the correlating group, epsilonLD 1/3, yields the curves in Fig. 1. The consolidated-sandstone correlation curve from Ref. 6 is reproduced here for comparison. Screen-factor losses resulting from mechanical degradation in unconsolidated porous media occur at larger values of epsilonLD 1/3 than in consolidated sandstones and are not well correlated; that is, this correlating group does not allow all screen-factor-loss data to converge on a single curve. SPEJ P. 172


Author(s):  
Huijun Zhao ◽  
Xiang Ding ◽  
Pengfei Yu ◽  
Yun Lei ◽  
Xiaofei Lv ◽  
...  

2015 ◽  
Vol 51 (2) ◽  
pp. 1036-1049 ◽  
Author(s):  
Jorge A. Ramirez ◽  
Andy J. Baird ◽  
Tom J. Coulthard ◽  
J. Michael Waddington

2016 ◽  
Vol 94 ◽  
pp. 422-432 ◽  
Author(s):  
N. Chikhi ◽  
R. Clavier ◽  
J.-P. Laurent ◽  
F. Fichot ◽  
M. Quintard

1981 ◽  
Vol 2 ◽  
pp. 115-115 ◽  
Author(s):  
D. G. Croot

Recent work by Clapperton (1975) proposes that the rapid rates of advance experienced by glaciers which surge may lead to enhanced debris incorporation, increased compressive flow near the glacier snout at the point of maximum extension, and to the upward translation and vertical stacking of debris near the glacier snout and margin. Five glaciers in Spitsbergen (Battyebreen, Holmströmbreen, Lisbetbreen, Vonbreen, Elnabreen) display morphological features which are widely accepted as being diagnostic of surging glaciers.Results of detailed observations regarding the nature, distribution, melt-out, and reworking of englacial debris at Battyebreen are presented. Basally derived till is brought to the surface of the glacier in narrow lateral and terminal belts, no more than 100 m wide. Within this zone, (i.e. up-valley from the snout and towards the valley centre) the ice is debris-free with the exception of small amounts of en-glacial debris which form the core of lobate medial moraines. Differential ablation of debris-free and debris-rich ice leads to the production of a topographic basin within which melt-out and reworking processes occupy restricted locations, as follows. Immediately inside the encircling melt-out till, a zone of flow tills is found. Melt streams are located at the foot of, the flow till-mantled slope, producing narrow (150 m wide) outwash trains, which merge into deltas. The central area of the topographic basin is occupied by a supraglacial lake.Observations of the remaining four locations confirm that other glaciers in the vicinity, which display similar characteristics associated with surging, are developing a stagnant-ice zone of identical appearance. The pattern of processes observed at Battyebreen is thus repeated at each site.A simple model of depositional landscape development is proposed for surging valley glaciers in a sub-polar environment.


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