2019
DOI: 10.1016/j.foreco.2018.05.040
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Stability of Pinus thunbergii between two contrasting stands at differing distances from the coastline

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Cited by 15 publications
(7 citation statements)
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“…trees were targeted (root system 1, root system 2) as shown in Figure 1. The trees grew in a coastal forest stretching 8 km to the west end of the Atsumi Peninsula, Tahara City, Aichi, Tokai District, Japan [32][33][34][35], and were replanted after heavy damage by Typhoon Vera in 1959 [32]. The soil was sandy in nature [36].…”
Section: Test Treesmentioning
confidence: 99%
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“…trees were targeted (root system 1, root system 2) as shown in Figure 1. The trees grew in a coastal forest stretching 8 km to the west end of the Atsumi Peninsula, Tahara City, Aichi, Tokai District, Japan [32][33][34][35], and were replanted after heavy damage by Typhoon Vera in 1959 [32]. The soil was sandy in nature [36].…”
Section: Test Treesmentioning
confidence: 99%
“…From 1981 to 2010, the mean annual temperature was 16.0 °C, and the mean annual precipitation was 1603 mm [37]. After measuring the tree height and DBH, we measured the critical turning moment in tree-pulling experiments using the method described by Todo et al [35] and cut the trees at the ground level. The tree-pulling experiment was performed as follows: a polyester belt sling (safe working load: 6.3 t) was attached to the tree, connected to a 10 mm diameter wire rope 1 m above the ground, and this was pulled, parallel to the ground, by an excavator.…”
Section: Test Treesmentioning
confidence: 99%
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“…Yet our understanding of coarse-root functions is poor. Todo et al (2018; this issue) investigated coarse-root anchorage in a Japanese coastal pine forest. The authors showed that the relationship between tree size and anchorage did not differ between land-side and sea-side plots, suggesting that the plate root systems of sea-side trees are acclimated to strong winds and the shallower ground water table: the lower critical turning moment of the plate-root system of sea-side pine trees is compensated for by enhanced horizontal root development.…”
Section: Future Challenges: Tsunamis Heavy Forest Equipment and Seedling Regenerationmentioning
confidence: 99%
“…Soil water deficits, due to deep groundwater levels, cause the dieback of trees at inland windbreaks under dry climates [6], whereas windbreaks can decline in vigor due to shallow groundwater at coastal sand dunes [7,8] and near paddy fields [9] in humid regions. High groundwater levels cause roots to remain shallow [10], reducing the resistance of coastal windbreaks to tsunamis [11]. Trees with shallow roots can be easily uprooted during a tsunami and carried to residential areas.…”
Section: Introductionmentioning
confidence: 99%