Report_GEO_ER-HWY-252_3.23.20.pdf

LUIS O. GARCIA & ASSOCIATES

GEOTECHNICAL ENGINEERING CONSULTANTS

Partners Luis Oscar García, MSCE, CE Carlos García Echevarría, MSCE

Associate Alejandro E. Soto, MS, PG

AMELIA DISTRIBUTION CENTER, EMMA STREET NO. 26A, GUAYNABO, PR 00968-8007

TEL. (787) 792-2626 FAX (787) 782-5990

Email: cgarcia@geocim.com

GEOTECHNICAL MEMORANDUM

TO : Dr. Eusebio Iglesias

Iglesias Vázquez & Associates iva@ivapr.com

FROM : Eng. Carlos García Echevarría, P.E.

Geol. Alejandro Soto, P.G.

RE : Landslide Evaluation PR-152, Km. 5.3-5.4, Barranquitas, PR

JOB NO. : 5160

DATE : January 28, 2019

This memorandum presents the results of a geotechnical investigation of a landslide that impacted State Road PR-152 at Kilometer 5.3 in the Quebradillas Ward of the municipality of

Barranquitas. The approximate location of the project site is shown in Figure 1 – Site Location

Map. The objective of the investigation was to evaluate subsoil conditions at the site in order to provide geotechnical recommendations for the design and construction of landslide stabilization alternatives that would enable the full reopening of PR-152. The Puerto Rico Highway and

Transportation Authority (PRHTA) are the project sponsors and Iglesias Vázquez & Associates

(IVA) are the Project Designers. The work was performed in general accordance with our proposal dated May 3, 2018. This report provides a summary of the activities performed during

Landslide at PR-152, Km. 5.3-5.4, Barranquitas, PR January 28, 2019.

the course of the investigation, a description of subsurface conditions encountered at the site, and geotechnical recommendations for the design and construction of landslide stabilization alternatives for the project.

At the project site various discontinuous landslides occurred along the inside edge of the roadway for approximately 300 feet (from about kilometers 5.3 to 5.4). At some of the landslide locations there was extensive amounts of soils that flowed down the slope causing damage to structures on the outside edge of the roadway. At the western portion of the site (location of boring B-1) it appears that some of the landslide debris remained on the slope as a portion of an existing electric pole seems to be buried; at this location there is a generally level area behind the existing slope adjacent to the roadway that extends about 50 to 60 feet and an approximately10 to 12 high, very steep landslide scar occur behind this level area. Concrete electric poles with an electric transmission line are supported mostly along the inside edge of the roadway which will require their relocation in orderto perform construction of stabilization alternatives at the site.

The geotechnical investigation performed consisted of the drilling three (3) borings (B-1 to B-3) to depths of 13.5 to 15 feet for a total of 43.5 lineal feet of drilling exploration; the originally proposed boring depths of 30 feet could not be attained as hard subsoil conditions were encountered providing refusal to the penetration of borings beyond their final depths. The location of the borings at the site was established in the field by GeoCim by visual observation from existing local references; the presence of underground and areal utilities in the area and vehicle traffic requirements on the roadway were also taken into consideration in the selection of the location of the boring. The approximate boring locations is shown on Figure 2 – Boring

Location Plan; all of the borings were on the inside edge of the PR-152 in the areas where the major landslides occurred. One of the borings could not be drilled in the intermediate area of one of the landslides due to access problems as the existing electrical transmission lines at the site laid very close to any access path that could have been opened with earthmoving equipment.

Geo Cim, Inc., our affiliate geotechnical testing services firm, performed the field and laboratory work. The borings were drilled with a CME-45 drill rig using the "Hollow Stem

Auger-Dry Sample" method of drilling and an Automatic SPT hammer. Soil samples were collected beginning at the ground surface, at 2.5-foot depth intervals to the bottom of the borings.

The samples were collected with a split-spoon sampler driven into the ground. The number of blows required to drive the split-spoon sampler into the soil was recorded in the field; the N-value of the SPT represents the number of blows required for the penetration of the last 12 inches of the sampler. The samples were placed in tightly closed plastic bottles and transported to the

GeoCim Geotechnical Testing Laboratory in Guaynabo for unconfined compression testing (in cohesive samples using a spring tester and/or pocket penetrometer), natural moisture content determinations, and visual/manual soil descriptions following standard laboratory procedures.

Three (3) Classification Tests, including Sieve Analysis and Atterberg Limits, were performed on selected samples from the borings. The results of the field operations, laboratory testing, and detailed descriptions of the soils encountered are documented in the boring log included in

Appendix A. Appendix B contains a description of the GeoCim, Inc. drilling, sampling, and testing procedures. Results of the Classification test is provided in Appendix C.

GEOLOGY AND SUBSOIL CONDITIONS

Figure 3 reproduces the portion of the Barranquitas geologic quadrangle map prepared by the U.S. Geological Survey (USGS) wherein the PR-152, Km 5.3 to 5.4 slope failures are located; the geologic units present in the area are distinguished by different colors and letter symbols.

The USGS identified two map units within the PR-152 Km. 5.3 to 5.4 road section

(Figure 3). The southern portion of the section was mapped as massive lava of Formation L (unit

Kl in reddish brown) of Cretaceous age (65+ million years old). The northern section traverses an area underlain by “tuffaceous sandstone and siltstone” identified as the volcaniclastic member of

Formation L (brown-colored unit labeled Klts), The volcaniclastic strata are shown to outcrop along the lower portion of the cut slopes on the east side of the roadway, with lava from unit Kl forming the upper slope. The siltstone-sandstone strata within the landslide section are shown to have an easterly dip of 28°.

The map shows these 2 geologic units to be in both fault (thick black line) and depositional (thin black line) contact. Three geologic faults are shown in the vicinity of the landslide section (Figure 3), two of which cross the roadway with a west-northwest trend some

200+ meters north of the landside section. The southernmost fault is shown to cross the impacted roadway section trending roughly east-west and forms part of the contact between the lava and volcaniclastic rock units. The fault is represented by a dashed line which reflects uncertainty as to its precise location, that is, the map maker was not able to trace the fault along the shown length but most likely connected several outcrops where a fault or features attributable to faulting were observed. We did not see this fault during our site reconnaissance. Rather, our observations indicate the volcaniclastic strata extend along the entire roadway section, making up the entire visible slope in its southern portion where the geologic map shows the lava unit; farther north, however, the siltstone-sandstone strata outcrop in the lower portion of the slope, with the lava unit forming the slope above it, as shown on the geologic map.

The exposed siltstone-sandstone strata consist of thin to medium (3 to 30 cm) beds that strike in a N20-30W direction while dipping around 20° to the northeast. Most of the individual strata are highly to moderately weathered and friable to moderately strong, with occasional thoroughly weathered, friable beds (the terminology used to describe the physical character of rock materials is explained in Table 1). This contrasts with the Formation L lava outcrops that typically consist of silty to clayey residual soil. Although the strong Hurricane María rains triggered landsliding in both types of geologic material, failures in the residual soil slopes were generally larger and more extensive than in the weathered rock strata.

As noted above, the 3 exploratory borings drilled along the landslide section were located along the inside (upslope) edge of the roadway; no borings were drilled on or above the roadway cut slopes due to access limitations. All 3 borings encountered similar subsurface profiles consisting of an upper 2-foot thick horizon of gravelly man-made fill followed by thoroughly to highly weathered, friable to weak sandstone or siltstone. The Fill layer is described as a Gravel with little to some clay or with little silt and sand in a medium dense to dense condition as indicated by N-values of 16 to 29 blows per foot (bpf), except in boring B-2 where N-value over

100 bpf was encountered probably due to an oversize gravel particle. This layer is probably the pavement base course material for the roadway.

The Thoroughly Weathered, friable to weak Sandstone or Siltstone is described as sampled as a Clay to clayey Sand to silty Sand in a very stiff to hard and dense to very dense condition as indicated by N-values of 25 to over 100 bpf with the N-values generally increase with increasing depth as would be expected in a residual soil profile where the soils are formed in-place by weathering and decomposition of the parent rock over geologic time. The higher penetration resistance (N-values over 100 bpf) obtained toward the bottom of the borings indicate virtual refusal to the penetration of the sampler; very hard conditions were encountered at the bottom of the borings which provided refusal to the penetration of the augers at depths of about 13.5 to 15 feet depth. Results of a Classification Tests performed on samples from the

Clay to clayey Sand to silty Sand layer at 2.5 to 5 feet depth indicate that it classifies as a low plasticity Clay (CL) to clayey Sand (SC) to silty Sand (SM) in accordance with the Unified Soil

Classification System with 41.3%to 59.9% of fines (passing the #200 sieve), and Liquid Limits

(LL) of 34% to 43% and Plasticity Index (PI) of 13% to 23%, except in boring B-3 where the sample indicated Non-Plastic characteristics. Ground water was not observed in the borings.

A detailed description of the soils encountered is provided in the boring log in Appendix

A. Groundwater observations were made during drilling operations or within the open borehole immediately after drilling operations were completed and the augers were removed from the ground. For more accurate determination of groundwater levels or to determine groundwater level variations under different conditions (at times of heavy rain, etc.) and on a long term basis, then installation of piezometers and observation wells and their monitoring during extended periods of time would be required.

ANALYSIS, CONCLUSIONS AND RECOMMENDATIONS

This section of the report presents our analysis, conclusions and recommendations based on the results of the geotechnical investigation and site reconnaissance performed at the site. It is important to note that the main objective of these recommendations is to provide stability to the in the landslide area adjacent to the roadway.

Based on the results of the borings drilled and the site reconnaissance performed we understand that the landslides on the inside edge of the roadway in this area were triggered by the heavy rain that fell during Hurricane Maria that saturated the surface soils on the slope increasing their weight while reducing their strength; additionally, erosion of the near surface soils may have also occurred due to uncontrolled surface water runoff over the top edge of the slope causing local undercutting of the slope. As previously mentioned in the report, in the area of boring B-1 an initial steep slope adjacent to the roadway leads to a relatively level area for about 50 to 60 feet which then leads to a steep slope of about 10 to 12 feet in height where the landslide scarp is observed; visual observations suggest that several feet of landslide debris and eroded soils have deposited within the initial slope adjacent to the roadway and on the following level area. In the areas where borings B-2 and B-3 are located, the landslides adjacent to the roadway raise steeply to heights of about 15 to 25 feet or more; they appear to be stable but long term stability of these steep to very steep slopes cannot be assured. The areas between the landslides that occur along this roadway segment have remained stable but their conditions could not be observed in detail because of dense vegetation cover; however, their long term stability cannot be assured (especially during events of heavy rain) because of their steep condition.

Several photos of the site obtained during our visit to the site on May 2018 are contained in

Appendix D.

The stabilization alternatives may include the following:

1. Re-grading of the slope areas with cut slopes not exceeding 1.5(H):1(V) inclination and/or re-construction of the slope with an engineered compacted Fill with final slopes not exceeding 2(H):1(V) that would bring that final cut/fill slope to the top of the existing cut slope and/or landslide scarp or beyond. Survey information obtained by the Designer will allow evaluation of the required cut/fill slope inclination and their extent. This re-grading will include excavation of any landslide debris and eroded soils deposited within the landslide area, specially in the area of boring B-1 directly behind the steep slope adjacent to the roadway; the required excavation must remove all the existing landslide debris/eroded soils on the landslide area until the natural in-situ soils are encountered, with the depth of excavation to be determined in the field by the Project Geotechnical

Engineer by visual observations as the excavations proceeds. The required Fill for the re-construction of the slope (if required) shall be constructed as described in the Earthwork

Recommendations section contained later in this report, including keying each fill layer into the in-situ soils to avoid creating a preferred surface of sliding.

2. Gravity retaining wall such as a Gabion or Concrete wall – this wall may be founded within 3 feet below the roadway level and at the inside edge of the roadway where the

Clay to silty Sand to clayey Sand (Thoroughly Weathered Volcanic Sandstone) is encountered in the borings in a very stiff to medium dense to dense condition. The height of the wall shall be selected such that the existing soils adjacent to the roadway may be retained without providing any additional stability measures toward the top of the existing cut slope as these may lie outside the limits of the roadway; alternatively, an engineered compacted fill at maximum inclinations of 2(H):1(V) may be constructed from the top of the wall to the edge of the existing cut slope at the top, but in this alternative any loose/deposited material on the slope must be removed/excavated until the firm in-situ natural soils are exposed for the construction of the engineered Fill as described in Alternative 1 above. An Allowable Soil Bearing Pressure of 4,500 pounds per square foot (psf) may be utilized at the recommended foundation level for the design of the retaining wall; PRHTA standard drawings for these walls may be utilized.

For a detailed design, the lateral pressures acting on the retaining wall shall be determined using a triangular earth pressure diagram acting on a vertical plane passing through the heel of the wall and extending from the bottom of the wall to the proposed ground surface. This triangular earth pressure diagram shall be calculated using an

“active” lateral earth pressure coefficient, Ka, and an angle of internal friction (Ø) of 32 degrees for the backfill material to be utilized; a unit weight (γ) of 130 pounds per cubic foot (pcf) may also be used for the backfill material behind the wall. Any other surcharge loads acting on the ground surface at or near the walls must be added to the previously mentioned earth pressures to determine the final design lateral loads acting on the walls.

The above lateral earth pressure recommendations assume that any cut excavation into the existing soils for the construction of the retaining wall will be performed at an inclination not steeper that 1(H):1(V) and that the backfill material behind the wall will consist of an engineered compacted fill constructed as described under the Earthwork

Recommendations section of this report. The backfill material within 10 feet from the wall shall be placed in 4 to 6 inch thick layers and compacted with light, hand operated compaction equipment to 90% of the maximum dry density as obtained in the Modified

Proctor Test (ASTM D 1557). The backfill material beyond 10 feet from the wall shall be placed in 8 to 12 inches thick layers and each layer compacted to 95% of the maximum dry density as obtained in the Modified Proctor Test (ASTM D 1557) using conventional compaction equipment.

We have also assumed that the design of the retaining wall will include a drainage system that will provide a fast and efficient way to collect and dispose of any water that may infiltrate behind the wall in order to prevent the development of unbalanced water forces behind the wall; a typical drainage system would include a free draining crushed stone layer behind the retaining wall separated from the backfill material by a geotextile filter fabric (such as Mirafi 140N or equivalent), and a perforated drainage pipe placed at the bottom of the wall and connected to a proper drainage outlet.

Alternatively, other types of drainage composites specifically manufactured for drainage behind retaining walls may be used.

Prior to beginning construction of the retaining wall, the foundation bearing surface for the wall shall be cleaned and any soil/rock disturbed during the excavation operations (or any time thereafter) shall be removed to provide an undisturbed soil/rock bearing surface. We recommend that a Geotechnical Engineer and/or Engineering

Geologist be present at the site when the landslide area is excavated in order to observe and confirm that the proposed excavation depths reach the recommended firm bearing surface; therefore, the final bearing surface for the retaining wall shall be determined in the field based on observations of the materials exposed by the excavation.

3. Reinforced concrete retaining wall – in this alternative a reinforced concrete retaining wall may be designed following the same recommendations provided above for the

Gravity Retaining Wall, including bearing on the very stiff Clay and medium dense to dense silty to clayey Sand layer at a minimum depths of 3 feet and the inclusion of adequate drainage measures behind the wall. Also, the height of the wall may be limited such that an engineered compacted fill at maximum inclinations of 2(H):1(V) may be constructed from the top of the wall to the edge of the existing slope at the top. This reinforced retaining wall may be constructed with the larger portion of the footing under the existing roadway (L-shape wall footing) in order to minimize the amount of excavation into the lower portion of the existing slope.

Earthwork Recommendations

The following general earthwork recommendations are provided for construction of any fill or backfill that may be required within the project in the landslide areas.

1. Prior to commencing construction the site shall be cleared and grubbed of vegetation cover and topsoil that may exist at the ground surface and any existing asphalt/concrete pavement from the existing roadway shall be demolished and removed from the site. After the clearing, grubbing, and demolition operations of the existing facilities are completed, and after any cut excavations and removal of loose/deposited material on the slope are performed, the exposed surfaces shall then be proof-rolled with several passes of a heavy vibratory roller to detect any soft soil spot that may have to be removed and to densify any surface soil that may have been disturbed during the clearing and grubbing, and/or cut excavation operations.

2- Excavations into the existing Clay and clayey to silty Sand near the ground surface may be performed with conventional excavating equipment including bulldozers and excavators as indicated by results of the borings. In the westernmost say 75 feet of the project site where the concrete barriers have been placed, less weathered rock conditions are encountered although with very close fractures; this material may be excavated with heavy duty bulldozers with rippers in open areas where this type equipment may access freely, but we estimate that most excavations in this area will require the use of rock excavating equipment, such as impact breakers, in limited areas of excavation.

3- Materials from required cuts at the site shall not be used as Fill at the site. Fill and/or backfill material to be used at the site shall consist of a non-expansive A-2-4 soil or better in accordance with the AASHTO (American Association of State Highway and Transportation

Officials) Soil Classification system. All fill within the site shall be placed as engineered compacted fill in 8 to 10 inch thick layers and each layer compacted to a minimum of 95% of the Maximum Dry Density as obtained in the Modified Proctor Test (ASTM D-1557); in excavations of limited extent the thickness of the fill layers placed shall be reduced to about 4 to 6 inches in order to attain the above compaction level. Fill required on sloped surfaces shall be placed in horizontal layers starting from the lower elevations and each horizontal layer shall be keyed into the in-situ soils so as to prevent the development of a preferred surface of sliding along the contact of the natural soils and the engineered compacted fill.

4- Temporary cut excavations on the in-situ soils deeper than 4 feet shall be performed with inclinations not steeper than 1(H):1(V); alternatively, the cut shall be properly braced and supported. Since bracing and support of cut excavations is a temporary construction feature, the Contractor shall design and select the most suitable support system for the excavation equipment and technique that he will use in the project.

5- We recommend that final cut and fill slopes (if any) be constructed at inclinations not to exceed 1.5(H): 1(V) and 2(H):1(V), respectively. All cut and fill slopes shall be properly and promptly vegetated in order to prevent excessive erosion of the soils that may cause instability of the slopes.

6- The project should be provided with adequate surface drainage measures to collect and conduct runoff to adequate discharge locations and/or to the storm water system of the existing PR-152 roadway. Under no circumstance should water be allowed to accumulate anywhere within the project or to spill over the recommended retaining walls and/or cut and fill slope embankments.

We request to be consulted should there be any questions on the intent and general scope of our recommendations. Likewise, we request to be informed of any changes in the scope of this project that may require our revision of these recommendations or if additional recommendations are needed.

N:\0000-project files\5160 Lanslide Evaluations IVA\PR-152 Km 5.4 Barranquitas\PR-152 Km 5.3 Landslide Report.doc

Figure 3: Portion of the Barranquitas geologic quadrangle map that shows the general geology of the PR-152

Km 5.3 to 5.4 Landslides area (the failures occurred on cut slopes on the east side of the road section between the arrows). The various map units are identified by different colors and letter symbols. There are 2 map units within the failure section: to the south are massive lavas of Formation L (unit Kl in reddish brown) and to the north are volcaniclastic strata of unit Klts (in brown), a clastic member of Formation L. The area shown is roughly 475 meters wide and the map contour interval is 10 meters; north is up. See report text for more information.

Kl

Table 1: Descriptive Terminology Used to Describe the Physical Properties of Rock for Engineering Purposes

WEATHERING CLASSIFICATION

Fresh No visible sign of weathering

Faintly Weathered Weathering limited to surface of major discontinuities

Slightly Weathered Penetrative weathering developed on open discontinuity surfaces, but only slight

Moderately Weathering extends through the rock mass, but rock is not friable

Highly Weathered Weathering extends through the rock mass and rock is partly friable

Thoroughly Rock is wholly decomposed and friable, retains rock structure and texture

Saprolite Soil that retains the original rock texture and structure

Residual Soil Soil with the original rock texture, structure and composition completely destroyed

FRACTURE SPACING

Fracturing Size Range of Rock Fragments

Crushed Less than 1.5 cm Intensely fractured 1.5 - 3.0 cm Closely fractured 3.0 – 15 cm

Moderately fractured 15 – 30 cm Little fractured 30 cm – 1 m

Massive Greater than 1 m

HARDNESS

Soft Plastic material

Friable Easily crumbled or powdered by fingers Low hardness Can be gouged deeply or carved with a knife

Moderately hard Can be readily scratched by a knife blade; scratch leave heavy trace of dust Hard Can be scratched with difficulty; scratch produces little powder and is faintly visible

Very hard Cannot be scratched with a knife blade

STRENGTH

Plastic Easily deformable with finger pressure Friable Crumbles by rubbing with fingers Weak Unfractured outcrop crumbles under light hammer blows

Moderately strong Outcrop withstands a few strong blows before breaking Strong Outcrop would withstand a few heavy ringing hammer blows, but will yield large fragments

Very strong Outcrop would resist heavy ringing hammer blows and yield dust and small fragments with difficulty

APPENDIX A

BORING LOGS

APPENDIX B

FIELD AND LABORATORY TEST PROCEDURES

GEO CIM, INC.

Appendix B

Field and Laboratory Test Procedures

I. DRILLING METHODS

A. Hollow Stem Auger Boring - Dry Sample method (ASTM-D-1452)

In the auger method, borings are advanced by turning a hydraulic powered auger into the ground in 5 feet increments or less. As the auger penetrates the cuttings rise to the surface on the spirals. The depth from which the material comes, however, cannot be accurately determined. Therefore, soil samples are not taken from the spiral augers. With the use of a hollow stem auger, a sampling apparatus may be inserted in the hollow stem to the bottom of the auger, eliminating the need for casings. The sampling procedures are described in the following paragraphs. Geo Cim, Inc. normally uses CME (Central Mining Equipment) drilling rigs which are trailer mounted and pulled with a 4 x 4 wheel drive F-350 or equivalent truck. The drilling rigs are either CME-45 or CME-55 models.

B. Wash Boring - Dry Sample Method

For inaccessible locations a portable drilling unit is used which consists of a tripod mounted motorized cathead which is used to drive casings and sampling rods to conduct this method of drilling. Borings are advanced into the ground by the wash-boring-dry sample method. The borings are normally cased through most of this length by the drop of either a 350 or 140 lbs. hammer from a height of 30 inches. The casing diameter is 2-1/2 inches. The number of blows for every foot of penetration the casing advanced is recorded and is reported in the boring logs. When driving of the casing becomes too difficult due to the hardness of the soils encountered, and the hole does not cave-in, the boring may be advances without casing by continuous washing out of the soils with the drill rods. The color and nature of the soils washed out (gravel, sand, silts or clay) is examined and recorded in order to determine the extent of each soil strata this is complemented with the sampling operations which are regularly made every five feet.

C. Core Borings (ASTM-D-2113)

Core Borings are used when necessary to penetrate into rock and obtain a continuous rock sample. The sample is obtained by means of a core barrel which is attached to the drill rods. At the end of the core barrel is a special bit studded with industrial diamonds which cuts into the rock. The drill rod, and hence the core barrel and diamond bit are rotated as downward pressure is applied. As the bit cuts into the rock, the rock core is free to move into the inner core barrel head, which is suspended on a swivel and therefore does not follow the motion of the outer core barrel with its bit. Cooling water or bentonite slurry is circulated through the drill rod and the core barrel. Penetration depends on the length of the core barrel and the quality of the rock (amount of joints or fractures). Rock discontinuities such as joints and fractures affect the length of penetration in a given core run. The runs are longer as the rock quality increases. As the core barrel is withdrawn, the core lifter, located inside the diamond bit, wedges itself around the bottom of the rock core and thus permits it to be pulled free from the underlying rock. The two most common core sizes are NWM which produces a core of 2.15 inches diameter and HWM which produces a core 3.00 inches in diameter.

II. SAMPLING IN SOILS

A. Standard Penetration Test (ASTM-D-1586)

The standard penetration tests are made with a split-spoon sampler 2.0 inches/O.D.

diameter, 1,375 inches I.D. diameter, 18 inches long. The sampler is driven into the ground by the drop of a 140 pounds hammer from a height of 30 inches. The number of blows from the three consecutive six inches of penetration of the sampler is recorded and the number of blows for the last foot of penetration is reported as the N-value. The samples are stored and sealed in glass jars for future classification tests in the laboratory.

The standard penetration test has been correlated with the consistency of fine grained soils and with the angle of internal friction or the relative density of sands. Such correlations can be used for preliminary estimates and to aid in the stratigraphic classification of the soil strata at a given site.

In the case of fine grained soils, the correlations of the SPT with the undrained shear strength of medium and stiff silts and clays of low sensitivity have been found to be fairly good; however, in the case of the soft silts and clays the SPT gives poor estimates of the undrained shear strength. Testing in undisturbed samples and vane shear tests are recommended in such cases.

B. Undisturbed Sampling

Undisturbed Samples are obtained using thin wall brass or zinc coated steel shelby tubes 2" to 3"O.D. by 24" to 30" long. The sampler is forced to penetrate the soil by static force or downward pressure and is pulled out also using static pull. The samplers are sealed in the field and shipped to the laboratory where the samples are extruded at the time of testing by pushing in the same direction that the sample penetrated the sampler. Special care is taken in packing and handling these samples to avoid disturbance.

III. LABORATORY TESTING

A. Atterberg Limits (ASTM-D-2166)

The Atterberg limits and related indices are very commonly used in soil mechanics works mainly for soil identification and classification purposes. They are also used in connection with some semi-empirical methods of design for preliminary estimates.

B. Unconfined Compression Test (ASTM-D-2166)

The best quality samples recovered in the split-spoon sampler are subjected to unconfined compression to failure. These samples cannot be regarded as “undisturbed” and the strengths obtained are lower than the “true” in-situ value due to the effect of disturbances and sensitivity of the soil. Furthermore, increased brittleness of friability of the soil structure results in strength values lower than the in-situ undrained strength.

Therefore, the unconfined strength values measured in the split-spoon samples are used only as an index property for classification and identification purposes. When more accurate values of strength are needed, undisturbed samples from thin-wall shelby tubes are used.

C. Natural Moisture Content (ASTM-D-2216)

The natural moisture content is the water content of the soil in-situ. The soil sample is obtained from the SPT sampler or shelby tubes. Approximately 40 gms. of soil are weighed and then placed in an oven for 24 hours at a temperature of 105� - 110�C. The natural moisture content, “Wn” is obtained from the difference between the weights in the natural state and after oven drying, divided by the dry weight of the sample and expressed in percentage.

IV. SOIL DESCRIPTION (ASTM-D-2488)

The description of the soils include the type (gravel, sand, silt, clay, organic), consistency (if a fine grained soil), size and roundness (if a coarse grained soil), color, and some other special characteristic which can aid in the identification and classification of the soil such as presence of rubbish, organic matter, shells and fossils, stratification and structure, cementation, mineral composition, relict structures, stains and others.

To aid in the preparation of these descriptions some simple tests are made such as those recommended by the Unified Soil Classification system for field classification (dilatancy, dry strength, shine, toughness). To approximate the consistency of fine grained soils (soft, medium, stiff, hard), a simple test is performed with the hand: a hard fine grained soil is difficult to indent with the thumbnail, stiff soils are readily indented with the thumb, medium soils can be penetrated by moderate thumb pressure and soft soils are easily penetrated with the thumb.

The description of coarse grained soils (sands and gravel) includes size (fine, medium coarse) and roundness (angular, sub-angular, sub-rounded, rounded and well-rounded).

The relative amount of coarse fractions in fine grained soils is estimated by placing a representative sample or some 50 gms. in a graduated cylinder filled with water. The mix is shaken and allowed to settle. Particles of a size larger than a fine sand are visible to the naked eye while silts and clays are not. In this manner, estimates of the relative amounts of the coarse fraction are made and reported as:

Trace 1 10% Little 10 20%

Some 20 35% Sandy, gravelly, silty or clayey 35 50%

The relative density of sands has been correlated with the results of the Standard

Penetration Test, as follows:

For Granular Soils N-Blows/ft. Relative Density

0 – 4 Very loose 4 – 10 Loose

10 – 30 Medium 30 – 50 Dense over 50 Very dense

These are very approximate correlations which vary with, among other factors, overburden pressure (Gibbs and Holtz, 1957, and Peck and Bazaraa, 1967). These correlations are meaningless in soils with a significant amount of gravel or cobbles.

The relative amounts of the fine grained soils is estimated based on the reaction of the soils to the dilatancy, shine, dry strength and toughness tests, with adjective indicating the less active fraction i.e. a sandy clay behaves more like a clay than a sand.

The consistency of cohesive soils has also been correlated to the results of the Standard Penetration Test, as shown below. The correlation, however, is greatly affected by the clay structure and factors such as sensitivity.

For Cohesive Soils

Unconfined Compressive Strength (T.S.F.)

N-Blows/Ft.

Consistency

Less than 0.25 Less than 2 Very soft

0.25 – 0.50 2 – 4 Soft

0.50 – 1.00 4 – 8 Medium

1.00 – 2.00 8 – 15 Stiff

2.00 – 4.00 15 – 30 Very stiff More than 4.00 More than 30 Hard

Once the soil samples have been tested, they are stored for three months after the date of our final report, and then destroyed, unless required in writing by the client to store them for a longer period.

APPENDIX C

CLASSIFICATION TEST REPORTS

APPENDIX D

SITE PHOTOS

H. MARIA LANDSLIDE SITES

Road # and Station: PR-152, Km 5.3 to 5.4, Barranquitas Client: iva

Site Photographs:

April 29, 2019

Iglesias Vázquez & Associates

320 Fortaleza Street

San Juan, P.R. 00902-4070

Attn.: Dr. Eusebio Iglesias iva@ivapr.com

Re: Addendum Letter to Geotechnical Report for Landslide Evaluation Located at

PR-152, Km. 5.3 - 5.4, Barranquitas, PR

ER-HWY-252, AC-807541

Dear Dr. Iglesias:

In our geotechnical report for the subsoil investigation, evaluations and recommendations regarding the landslide at the above referenced site, we have evaluated the stability of the proposed geotechnical alternatives based on our experience, subsurface conditions encountered at the site and evaluation of allowable soil bearing pressures on the recommended bearing strata.

Additional analysis regarding the stability of the final selected alternative at this site will also be performed during the final design stage of the selected alternative when final dimensions and depth of the retaining structures are established.

Cordially, Carlos García Echevarría, P.E.

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PR-152 km 5.3 - 5.4 Barranquitas.doc

May 6, 2019.

Iglesias Vazquez & Associates

320 Calle Fortaleza

San Juan, PR

Attn.: Dr. Eusebio Iglesias iva@ivapr.com

Re.: Geotechnical Reports for Landslide Projects due to María Hurricane at Various Locations in Puerto Rico

Dear Dr. Iglesias:

As requested by you and in response to comments that you received from ACT to our geotechnical reports for the above referenced projects, the recommended 1(H):1(V) temporary cut excavations inclinations for the proposed project were re-evaluated after Iglesias Vazquez &

Associates (IVA) indicated that construction of the proposed retaining structures would require a steeper slope in order to prevent the closure of the roadway during construction. Based on the type of subsoils encountered at the projects and observations in nearby areas where these soils stand at higher inclinations, we then recommended that temporary cut excavations at these sites may be performed at inclinations not steeper than 1(H):1.5(V); alternatively, the cut excavation shall be properly braced and supported as indicated in the Geotechnical Memorandum. All excavations shall be performed in general accordance with requirements in OSHA CFR 1926

Subpart P – Excavations.

As indicated in the Geotechnical Memorandum, a Geotechnical Engineer or Engineering

Geologist shall be present at the site during the excavation work in order to observe and confirm the type of materials exposed and that an adequate bearing surface is reached.

If you have any questions, please do not hesitate to contact me.

Cordially, Carlos García Echevarría, P.E.

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