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Undrained Load Capacity of Torpedo Anchors in ... - laceo - UFRJ

Undrained Load Capacity of Torpedo Anchors in ... - laceo - UFRJ

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total vertical load unable to pull the anchor out. On the<br />

contrary, for <strong>in</strong>cl<strong>in</strong>ations higher than 45°, a small amount <strong>of</strong><br />

soil is mobilized, but the reduction <strong>in</strong> the surround<strong>in</strong>g soil<br />

stiffness and the high vertical loads are enough to pull the<br />

anchor out and well characterize its load capacity.<br />

It is worth mention<strong>in</strong>g that the differences between the<br />

observed failure mechanisms make the determ<strong>in</strong>ation <strong>of</strong> the<br />

anchor hold capacity a difficult task. On the one hand, for<br />

<strong>in</strong>cl<strong>in</strong>ations higher than 45°, the failure is clear and the hold<br />

capacity is well determ<strong>in</strong>ed. On the other hand, for <strong>in</strong>cl<strong>in</strong>ations<br />

lower than 45°, the failure is not clear and a criterion should be<br />

established to determ<strong>in</strong>e the load capacity. One possible<br />

criterion would be the maximum total displacement reached.<br />

However, Figs. 12 to 14 po<strong>in</strong>t a significant variation <strong>of</strong> the<br />

maxima displacements achieved <strong>in</strong> each analysis. When<br />

horizontal loads are applied, displacements <strong>of</strong> about 25cm are<br />

verified, while, when vertical loads are applied, these values<br />

may be as low as 5cm. Hence, this seems to be not a suitable<br />

choice and more studies must be performed to tackle this issue.<br />

In this work, <strong>in</strong> the lack <strong>of</strong> a def<strong>in</strong>ed criterion, the<br />

maximum load achieved <strong>in</strong> each FE analysis is considered to be<br />

the hold capacity <strong>of</strong> the anchor hereafter. Thus, Tables 2 to 4<br />

present the calculated load capacities for soils A, B and C.<br />

<strong>Load</strong><br />

<strong>in</strong>cl<strong>in</strong>ation<br />

Table 2 – <strong>Load</strong> capacities for soil A.<br />

<strong>Load</strong> Horizontal<br />

capacity component<br />

(kN) (kN)<br />

Vertical<br />

component<br />

(kN)<br />

0° 5900 5900 -<br />

15° 6075 5868 1572<br />

30° 6413 5553 3206<br />

45° 6628 4687 4687<br />

60° 5981 2991 5180<br />

75° 5325 1378 5144<br />

90° 5176 - 5176<br />

API 5241 - 5241<br />

<strong>Load</strong><br />

<strong>in</strong>cl<strong>in</strong>ation<br />

Table 3 – <strong>Load</strong> capacities for soil B.<br />

<strong>Load</strong> Horizontal<br />

capacity component<br />

(kN) (kN)<br />

Vertical<br />

component<br />

(kN)<br />

0° 11719 11719 -<br />

15° 11869 11464 3072<br />

30° 12280 10635 6140<br />

45° 10526 7443 7443<br />

60° 8916 4458 7721<br />

75° 7950 2058 7679<br />

90° 7756 - 7756<br />

API 7163 - 7163<br />

<strong>Load</strong><br />

<strong>in</strong>cl<strong>in</strong>ation<br />

Table 4 – <strong>Load</strong> capacities for soil C.<br />

<strong>Load</strong> Horizontal<br />

capacity component<br />

(kN) (kN)<br />

Vertical<br />

component<br />

(kN)<br />

0° 20984 20984 -<br />

15° 21608 20872 5593<br />

30° 20414 17679 10207<br />

45° 15694 11097 11097<br />

60° 12958 6479 11222<br />

75° 11850 3067 11446<br />

90° 11456 - 11456<br />

API 10018 - 10018<br />

For soil A, Table 2 shows that the load capacity <strong>in</strong>creases<br />

with the load <strong>in</strong>cl<strong>in</strong>ation until the maximum value is reached at<br />

an angle <strong>of</strong> 45°. After that, the load capacity is reduced until the<br />

m<strong>in</strong>imum value is reached for an <strong>in</strong>cl<strong>in</strong>ation <strong>of</strong> 90°. For soil B,<br />

a similar behavior was observed, but the maximum load<br />

capacity is obta<strong>in</strong>ed at a load <strong>in</strong>cl<strong>in</strong>ation <strong>of</strong> 30° and the<br />

m<strong>in</strong>imum at 90°. For soil C, the maximum value occurs at an<br />

<strong>in</strong>cl<strong>in</strong>ation <strong>of</strong> 15° and the m<strong>in</strong>imum, aga<strong>in</strong>, at 90°.<br />

These tables also <strong>in</strong>dicate that the <strong>in</strong>crease <strong>of</strong> the undra<strong>in</strong>ed<br />

shear strength leads to an <strong>in</strong>crease <strong>in</strong> the load capacity <strong>of</strong> the<br />

anchor. However, this <strong>in</strong>crease is higher for lower load<br />

<strong>in</strong>cl<strong>in</strong>ations (between 0° and 15°) than for higher <strong>in</strong>cl<strong>in</strong>ations.<br />

For lower <strong>in</strong>cl<strong>in</strong>ations, the <strong>in</strong>crease <strong>of</strong> the undra<strong>in</strong>ed shear<br />

strength provoked an augment <strong>of</strong> the load capacity almost <strong>in</strong><br />

the same proportions, as the failure mechanism is directly<br />

related to the lateral resistance <strong>of</strong> the soil. For higher<br />

<strong>in</strong>cl<strong>in</strong>ations, the <strong>in</strong>crease <strong>of</strong> the undra<strong>in</strong>ed shear strength<br />

implies the reduction <strong>of</strong> the adhesion factor, α, Eq. (21), which<br />

reduces the effect <strong>of</strong> the augment <strong>of</strong> the undra<strong>in</strong>ed shear<br />

strength by reduc<strong>in</strong>g the limit<strong>in</strong>g shear stress on the <strong>in</strong>terface<br />

anchor-soil. As, for these <strong>in</strong>cl<strong>in</strong>ations, the load capacity is<br />

largely dependent on the adhesion between the soil and the<br />

anchor, the load capacity for higher angles is less affected by<br />

the <strong>in</strong>crease <strong>in</strong> the undra<strong>in</strong>ed shear strength <strong>of</strong> the soil.<br />

Moreover, the <strong>in</strong>crease <strong>of</strong> the undra<strong>in</strong>ed shear strength<br />

amplifies the difference between the horizontal and the vertical<br />

load capacities. For soil A, the horizontal capacity is 14%<br />

higher than the vertical one. For soils B and C, these differences<br />

are, respectively, 51% and 83%.<br />

Tables 2 to 4 also present the horizontal and vertical<br />

components <strong>of</strong> each obta<strong>in</strong>ed load capacity. These values po<strong>in</strong>t<br />

that, for <strong>in</strong>cl<strong>in</strong>ations lower than 30°, the horizontal components<br />

are close to horizontal load capacity. On the contrary, for<br />

higher <strong>in</strong>cl<strong>in</strong>ations, the vertical components are almost<br />

co<strong>in</strong>cident with the vertical load capacity. This is consistent<br />

with the described failure mechanisms.<br />

As a consequence, the load capacities <strong>of</strong> torpedo anchors<br />

subjected to loads with <strong>in</strong>cl<strong>in</strong>ations higher than 30° can be<br />

estimated by calculat<strong>in</strong>g the vertical load capacity <strong>of</strong> the anchor<br />

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