Potential bioavailability of representative pyrogenic organic matter compounds in comparison to natural dissolved organic matter pools by E. B. Graham, E. B. Graham, H.-S. Song, S. Grieger, S. Grieger, V. A. Garayburu-Caruso, V. A. Garayburu-Caruso, J. C. Stegen, J. C. Stegen, K. D. Bladon, A. N. Myers-Pigg, A. N. Myers-Pigg, A. N. Myers-Pigg

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Maximum respiration rates in hyporheic zone sediments are primarily constrained by organic carbon concentration and secondarily by organic matter chemistry by J. C. Stegen, V. A. Garayburu-Caruso, R. E. Danczak, A. E. Goldman, L. Renteria, J. M. Torgeson, J. Hager, J. Hager

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A multirate mass transfer model to represent the interaction of multicomponent biogeochemical processes between surface water and hyporheic zones (SWAT-MRMT-R 1.0) by Y. Fang, X. Chen, J. Gomez Velez, X. Zhang, Z. Duan, G. E. Hammond, A. E. Goldman, V. A. Garayburu-Caruso, E. B. Graham

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Disturbance triggers non-linear microbe–environment feedbacks by A. Sengupta, S. J. Fansler, R. K. Chu, R. E. Danczak, V. A. Garayburu-Caruso, L. Renteria, H.-S. Song, J. Toyoda, J. Wells, J. C. Stegen

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Organic matter transformations are disconnected between surface water and the hyporheic zone by J. C. Stegen, S. J. Fansler, M. M. Tfaily, V. A. Garayburu-Caruso, A. E. Goldman, R. E. Danczak, R. K. Chu, L. Renteria, J. Tagestad, J. Toyoda

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