Abstract

Descriptions of tree root morphology inform design of belowground biomass and carbon inventories and sampling for research. We studied root morphology of tanoak (Notholithocarpus densiflorus), an important component in mixed evergreen forests of California and Oregon, USA. Tanoak re-sprouts from belowground lignotubers after disturbances, and stores an unknown amount of carbon in coarse roots underground. We sought to ascribe explanatory nomenclature to roots’ morphological features and to identify models describing tanoak root morphology. Twelve tanoak root systems were excavated, dissected, and measured. Roots tapered according to their circumference and location. Larger roots closer to the lignotuber (located at the base of the tree stem) tapered more rapidly per unit of length. Tanoak roots forked frequently. Root cross-sectional area was preserved after forking events (i.e., the sum of cross-sectional areas for smaller roots on one side of the fork correlated with the adjoining large root). Occurrence and quantity of root branches (small roots branching laterally from larger roots) was dependent upon length of the source root segment. Our models of tanoak root morphology are designed to be organized together to estimate biomass of any segment or collection of lateral roots (e.g., roots lost/missed during excavation, or in lieu of destructive sampling), given root diameter at a known distance from the lignotuber. The taper model gives distal- and proximal-end diameters for calculation of volume for segments of root tapering between forks. Frequency of forking and branching can also be predicted. Summing the predicted mass of each lateral root segment, branch, and forked segment would produce an estimate of mass for a contiguous network of lateral roots.

Highlights

  • Tree roots are difficult to access and study, yet their important contribution to terrestrial carbon pools should be quantified

  • The excavated tanoak root systems had a threedimensional form described as a “heart” system, where horizontal and vertical roots develop from the base of the tree (Stokes & Mattheck, 1996)

  • Root taper is an important facet of root morphology

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Summary

Introduction

Tree roots are difficult to access and study, yet their important contribution to terrestrial carbon pools should be quantified. Estimates of tree root biomass and carbon content allow us to quantify impacts of land-use change and disturbances on belowground carbon pools. Tree root biomass sampling is challenging due to roots’ variable spatial distribution (Danjon & Reubens, 2008). Measuring the biomass of an entire root system requires complete excavation of the roots or removal of all soil surrounding them. An excavator can be used to remove the root-soil plate (a mass of woody tissue connecting the stem to the lateral roots), but hand tools or an air spade are required to excavate smaller more fragile roots (Bingham et al, 2001; Lavigne & Krasowski, 2007). Deriving total belowground biomass estimates from the excavated portions of a root system requires development of predictive models to account for the roots lost during the excavation process (Richardson & Dohna, 2003; Danjon et al, 2013)

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