Meinhard Bayani Cardenas first came to the United States from the Philippines just over 10 years ago and began studying stream-aquifer interaction during his M.S. at the University of Nebraska. Working with Vitaly Zlonik, he conducted an innovative field observational program, sampling hundreds of points within a streambed, which he used to examine the role of sediment heterogeneity on stream-aquifer interaction. Bayani then joined me at the New Mexico Institute of Mining and Technology for his Ph.D. Initially, we planned some field observations, but serendipitously, funding did not work out. He turned to mathematical modeling of the hyporheic zone, for which he is best known, and received his Ph.D. 6 years ago. Bayani moved to the University of Texas at Austin (UT), where he is an assistant professor in the department of geological sciences. Upon arrival at UT he continued his modeling work, returned to the field (including innovative applications of geophysical tools), added a strong laboratory component (he built his own flume), and published. Most important, he began to teach and to mentor students. The second page of his CV lists the honors won not by him but by his students.
In his work, Bayani examines the scales, rates, and residence times of hyporheic flow that are generated by a single downed log in a mountain stream, by bedforms lining the bottom of a sandy river, and by the pattern of river meanders. He has studied heat transport and ecologically important patterns of temperature in streams and hyporheic zones and has investigated reactive chemistry issues of importance to nutrient utilization in streams. However, his work does not stop there. He used his skill set to examine groundwater flow at the small scale of a few pores in order to understand how solutes are sequestered in porous and fractured rocks, leading to tailing of solute breakthrough, and at the large scale of a regional aquifer to understand that groundwater age distributions also exhibit tailing due to mixing between fast and slow flow paths even in homogeneous aquifers. A consistent theme of this work is the emergence of power law scaling of residence times over all scales and with a variety of contributing and complementary explanations. Aquifer heterogeneity is not required.
—Jonh L. Wilson, New Mexico Institute of Mining and Technology, Socorro