Static mixer KMX-V series
continuousfor liquidspolymer

Static mixer - KMX-V series - NOV Inc. - continuous / for liquids / polymer
Static mixer - KMX-V series - NOV Inc. - continuous / for liquids / polymer
Static mixer - KMX-V series - NOV Inc. - continuous / for liquids / polymer - image - 2
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Characteristics

Technology
static
Batch/continuous
continuous
Product type
for liquids
Applications
polymer

Description

The KMX-V static mixer is the best choice for demanding mixing applications, such a those involving fluids with extreme viscosity or volume ratios. PRINCIPLES OF OPERATION The KMX-V utilizes cross-stream mixing and flow splitting to achieve very rapid blending. Each element is approximately one pipe diameter in length and consists of multiple intersecting blades, which generate fluid layers as the mixture flows downstream. Each blade features concave construction offering better cross-stream flow than flat blades for superior mixing per unit length in tough, high viscosity ratio applications. Sheets of low viscosity additives are driven along the trough of each blade and abruptly sheared by strong cross-stream velocity gradients as they pass around the upstream surface. LAMINAR BLENDING As the additive enters the mixer, it is driven along the trough of each blade. At each blade intersection, the additive is sheared by strong cross-stream velocity gradients as it passes around the upstream surface. This mixing mechanism occurs thousands of times within a short mixing length. The result is that the additive is sheared into continuously finer striations and distributed evenly through the pipe and into viscous main fluid. HEAD-TO-HEAD COMPARISON Lab tests have proven that the concave surfaces of the KMX-V element promote more cross-stream flow than competitive designs with flat blades. This feature enhances the performance of the mixer in tough high viscosity ratio applications. Sheets of low viscosity additives are driven along the trough of each blade and abruptly sheared by strong cross-stream velocity gradients as they pass around the upstream surface.

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