Method Article

Laboratory and Field Protocol for Estimating Sheet Erosion Rates from Dendrogeomorphology

DOI:

10.3791/57987

January 7th, 2019

In This Article

Summary

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Characterizing erosion from dendrogeomorphology has usually focused on accurately finding the starting time of root exposure, by examining macroscopic or cell level changes caused by exposure. Here, we offer a detailed description of different novel techniques to obtain more precise erosion rates from highly accurate microtopographic data.

Abstract

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Sheet erosion is among the crucial drivers of soil degradation. Erosion is controlled by environmental factors and human activities, which often lead to severe environmental impacts. The understanding of sheet erosion is, consequently, a worldwide issue with implications for both environment and economies. However, the knowledge on how erosion evolves in space and time is still limited, as well as its effects on the environment. Below, we explain a new dendrogeomorphological protocol for deriving eroded soil thickness (Ex) by acquiring accurate microtopographic data using both terrestrial laser scanning (TLS) and microtopographic profile gauges. Additionally, standard dendrogeomorphic procedures, dependent on anatomical variations in root rings, are utilized to establish the timing of exposure. Both TLS and microtopographic profile gauges are used to obtain ground surface profiles, from which Ex is estimated after the threshold distance (TD) is determined, i.e., the distance between the root and the sediment knickpoint, which allows defining the lowering of the ground surface caused by sheet erosion. For each profile, we measured the height between the topside of the root and a virtual plane tangential to the ground surface. In this way, we intended to avoid small-scale impacts of soil deformation, which may be due to pressures exerted by the root system, or by the arrangement of exposed roots. This may provoke small amounts of soil sedimentation or erosion depending on how they physically affect the surface runoff. We demonstrate that an adequate microtopographic characterization of exposed roots and their associated ground surface is very valuable to obtain accurate erosion rates. This finding could be utilized to develop the best management practices designed to eventually halt or perhaps, at least, lessen soil erosion, so that more sustainable management policies can be put into practice.

Introduction

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Both economic and environmental impacts produced by sheet erosion makes this topic in a worldwide concern1. Several methods, from direct techniques to physical-based and empirical approaches, are used to calculate soil erosion rates on a variety of temporal and spatial scales. Direct techniques use field measurements under natural conditions and are mainly based on the use of Gerlach troughs2, water collectors3, erosion pins4 and profilometers5. Furthermore, models of soil erosion have been increasingly focused on representing in detail the real phys....

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Protocol

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1. Sampling Strategy

  1. Geomorphic process identification
    1. Implement the Hydrologic Response Units approach (HRU)21. To this end, identify homogenous areas within the study site, comprising lithology and surface deposits, canopy cover, vegetative residue in contact with the soil surface and slope. Select among all the HRUs those in which the sheet erosion process is predominant.

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Results

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Samples of exposed roots suffer serious cambial deterioration due to the impact of exposure (e.g., modifications in temperature, incidence of light) plus the physical stress, due to trampling by hikers or animal grazing and browsing that the roots undergo after they are exposed. Determining the existence of discontinuous rings, as well as precisely dating the first year of response to exposure was accomplished in the lab as in Protocol 4 (steps 4.1.6 to 4.1.8). We chose the incre.......

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Discussion

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The protocol deployed demonstrates the value of detailed and proper characterization of ground surface microtopography, as it enables to measure trustworthy sheet erosion rates from dendrogeomorphology. Our methodological approach focuses on the importance of characterizing the microtopography in the surroundings of exposure roots to improve erosion rate estimation. This factor has been largely ignored in previous studies, resulting in a misinterpretation of soil erosion rates derived from dendrogeomorphology

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Disclosures

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The authors have nothing to disclose.

Acknowledgements

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The research projects that funded this research were: MARCoNI (CGL2013-42728-R); Dendro-Avenidas (CGL2007-62063); MAS Dendro-Avenidas (CGL2010-19274) of the Spanish Ministry of Science and Technology and the project IDEA-GESPPNN (OAPN 163/2010), which was funded by the Environmental Ministry of Spain.

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Materials

List of materials used in this article
NameCompanyCatalog NumberComments
Topographic map, soil map, land cover mapTo be obtained from public institutions or generate at the first phase of research
Single ring infiltometerTurf-Tec InternationalIN16-Whttp://www.turf-tec.com/IN16Lit.html
HandsawThere is noy any specific characteristics to be considered regarding the model
Measuring tapeWith accuracy of 1 mm
Terrestrial Laser Scanning (TLS)Leica-GeosystemsLeica ScanStation P16https://leica-geosystems.com/products/laser-scanners/scanners/leica-scanstation-p16
Microtopographic Profile GaugeRS OnlineFacom, 19https://www.classic-conservation.com/es/herramientas-para-talla-y-escultura-en-madera/511-galga-medidora-de-perfiles.html
Sandpaperfrom 80 to 400 grit
ScannerEPSONPerfection V800 Photohttps://www.epson.co.uk/products/scanners/consumer-scanners/perfection-v800-photo
Image analysis systemRegent Instruments Inc.WinDENDROhttp://www.regentinstruments.com/assets/windendro_analysisprocess.html
Measuring tableIMLhttps://www.iml-service.com/product/iml-measuringtable/
Sliding microtomeThermo Fisher SCIENTIFICMicrom HM 450-387760http://www.thermofisher.com/order/catalog/product/910020
Optical microscopeOLYMPUSMX63/MX63Lhttps://www.olympus-ims.com/en/microscope/mx63l/
Digital camera for microscopeOLYMPUSDP74https://www.olympus-ims.com/en/microscope/dc/
SafraninEmpirical Formula (Hill Notation) C20H19ClN4 
AstrablueEmpirical Formula C47H52CuN14O6S3
AlcoholAlcohol by volume (50%, 75% and 100%)
Distilled waterH2O
Citrus oil clearing agenthttps://www.nationaldiagnostics.com/histology/product/histo-clear
Coated slidesThermo Fisher SCIENTIFIChttps://www.fishersci.com/us/en/products/I9C8JXMT/coated-glass-microscope-slides.html
Hardening epoxyMERCKhttps://www.sigmaaldrich.com/catalog/product/sial/03989?lang=es®ion=ES

References

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  1. Montgomery, D. R. Soil erosion and agricultural sustainability. Proceedings of the National Academic of Sciences of the United States of America. 104 (33), 13268-13272 (2007).
  2. Novara, A., Gristina, L., Saladino, S. S., Santoro, A., Cerdà, A. Soil erosion assessment on tillage and alternative soil managements in a Sicilian viney....

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Tags

Terrestrial Laser ScanningMicrotopographic Profile GaugeRoot Exposure TimingTree Ring AnalysisGround Surface MicrotopographySoil Erosion RatesExposed Root SamplingImage Analysis System

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