Operation Hardtack I

There was some uncertainty on whether detonating a nuclear weapon at such high altitudes would cause a hole in the ozone layer. After multiple underwater tests there was evidence to show the energy created by the blast would create ozone. Project leads determined some destruction of ozone would occur which would then be replaced by the ozone created from the explosion. It was agreed that if this theory were wrong, the hole created in the ozone layer would be minuscule enough to cause no harm. Upon completion of Operation Newsreel, it was determined that there was very little evidence of any harm being caused to the natural ozone layer.[5]

Yucca was the first high-altitude test performed during Operation Hardtack I and was detonated on April 28, 1958. It was lifted by a balloon to an altitude of 86,000 feet (26.2 km) and had a yield of 1.7 kilotons.[3]^:2[4]^:251To achieve the altitude needed, the device was attached to a large helium-filled balloon which carried it to the detonation altitude. Due to issues with high winds on Enewetak Island, the balloon launches from ground were unsatisfactory, thus creating the need for a new method. The balloons were then deployed from an aircraft carrier which helped with deployment and the inflation. While the balloons were inflated, they were unable to take too much force from wind or the plastic material of the balloons would tear. While the balloons were inflating on the aircraft carrier, the ship could match and oppose the wind speed allowing for the balloon to be inflated in still air. To make sure the launch would be successful 86 balloon launches were tested.[4]^:252

Due to concerns of failures, many safety measures were employed. While on ground, the bomb used multiple pins to prevent certain safety features of the bomb from being deployed before liftoff. One such pin was used to stop the electrical systems so that the bomb would be unable to be armed. In case of a dud, the bomb would detach from the balloon and be allowed to drop into the ocean where many more safety features would come into action. Some of these features included probes which could detect saltwater which would destroy the electrical system so the conductive seawater could not cause a short which would detonate the bomb. Another concern was a nuclear device floating in the ocean should a misfire occur. To combat this, inserts were created which would dissolve in a few hours, thus scuttling the device.[4]^:253–4

On the day of the launch many meteorological aspects were taken into account and calculations were done to ensure the bomb would reach the correct altitude. The bomb was loaded onto an aircraft carrier and preparations began. As the balloon was inflated multiple testing devices were connected to the balloon. The readings from these devices would be sent to multiple ships and aircraft so nothing would need to be recovered after the explosion. After all the preparations were done and the balloon was inflated, the device was released and began to climb. After almost three and a half hours of climbing the bomb was detonated at an altitude of 26.2 kilometers (16.3 mi). The aircraft carrier which carried Yucca was approximately 4 kilometers (2.5 mi) from the detonation site. The shock wave from Yucca reached the carrier 3 minutes and 16 seconds after detonation.[4]^:255–7

The Yucca test had many Department of Defense projects attached to it for research purposes. Alongside testing the use of a balloon carrier, the Department of Defense wanted to research the electromagnetic waves emitted from a nuclear explosion. This test would be used to determine the impact a nuclear explosion would have on electronic devices. All of the data from these Department of Defense projects would be stored on recording devices on surrounding islands and in aircraft so data would not have to be recovered after the test.[4]^:253–4 However, Yucca was carrying five different transmitting devices in canisters to help with research. While the balloon proved to be a great success, no data from the canisters were able to be retrieved due to equipment issues onboard one of the aircraft carriers.[6]^:201

The Teak test was launched from Johnston Island on July 31, 1958 and carried a payload of 3.8 megatons.[3]^:3[4]^:251 Teak was the second high-altitude test after the success of Yucca. Instead of a balloon, the warhead for the Teak test would be carried by a Redstone missile; a modified Redstone missile had been used to launch Explorer I in January of the same year.[4]^:256–7 Other nuclear weapons had been tested using the Redstone missile, but until this time the highest payload to have been detonated was 3 kilotons during Operation Teapot.[6]^:218 Teak would be the first high-altitude test to have a payload in the megaton range. The test was scheduled to take place from the Bikini Atoll. Due to the fact that the payloads of Teak and Orange were much larger than previous high-altitude shots, the test was moved to Johnston Island as to protect nearby native islanders from any retinal damage. As both Teak and Orange had been relocated these two tests were named Operation Newsreel. The name Newsreel came from the fact that these two tests were being moved to Johnston Island.[4]^:259

The safety precautions taken by the teams involved were precisely detailed. The day before the launch 187 team members would evacuate Johnston Island with 727 men the day of the test. This was to keep as few men on the island while still being able to operate the airfield and critical data instruments. Another problem the team members were concerned about was the issue of retinal damage. Since the payload of the bomb was so large, aircraft were scheduled to keep any civilian ships out of a 760 kilometers (470 mi) radius of Johnston Island. Additionally, the Civil Aeronautics Authority was informed that it would be dangerous for any aircraft to fly within 965 kilometers (600 mi) of Johnston Island. On the day of the test only about 175 men remained on Johnston Island to prepare for Teak to be launched and other various duties needed after.[4]^:262–3

At 11:47 PM on July 31 Teak was launched; after 3 minutes it was detonated. Due to programming issues, the warhead detonated directly above Johnston Island.[6]^:219 At time of detonation the rocket had flown to an altitude of 76.2 kilometers (47.3 mi). The explosion could be seen from Hawaii 1,297 kilometers (806 mi) away and was said to be visible for almost half an hour. After the explosion, high frequency long distance communication was interrupted across the Pacific. Due to this communication failure Johnston Island was unable to contact their superiors to advise of the test results until about eight hours after the detonation. Thirty minutes after detonation, a crew was sent out to collect the pod which had detached from the missile carrying the warhead. The pod had been irradiated and to handle it the crew members used disposable gloves in an attempt to protect themselves from beta radiation.[4]^:265–70

During the Teak test all crew on and around Johnston Island were given protective eyewear to prevent flash blindness from the explosion. After the explosion it was found that besides the hazard of blindness, thermal radiation was another concern—even at an altitude of 76 kilometers (47 mi). A crew member who was on Johnston Island at the time was said to have received a slight sunburn from the amount of thermal radiation which had reached the island. While only slight to the crew member it created issues for the local fauna. Many birds were seen on Johnston Island in distress. Unsure if this was caused by blindness or thermal radiation, the project members decided to take precautions to protect local wildlife during the Orange test.[5]

Orange was launched twelve days after Teak on August 11, 1958.[4]^:251 Orange, like Teak, was launched using a Redstone Missile and had a yield of 3.8 megatons.[3]^:3[4]^:271 The same safety precautions used by Teak were implemented for the Orange launch. Seeing how smoothly the evacuation for the Teak launch went, it was decided that the evacuation did not need to occur the day before the launch and eight hundred and eight men were evacuated on August 11 to an aircraft carrier about 70 kilometers (43 mi) northeast of the island. Along with protection for the project crew, it was decided after Teak that Sand Island, a local bird refuge, would need protection from the blast as well. To make sure that most of the wildlife was safe a smoke screen was created over Sand Island. Due to interest in Hawaii, it was announced on August 11 that there would be a nuclear test sometime between 10 PM and 6 AM.[4]^:271

The rocket carrying the warhead was launched at 11:27 from Johnston Island and traveled south. Like Teak, the flight lasted 3 minutes and was detonated at 11:30 PM about 41 kilometers (25 mi) south of Johnston Island at an altitude of about 43 kilometers (27 mi).[4]^:271The trajectory of Orange was a major success after the incident with Teak being detonated directly over the island.[6]^:219 The recovery crew for the pod that was with Orange was unable to locate the research pod which had been launched with the rocket. Although Orange was visible from Hawaii it was not the great spectacle Teak had been. The light from the blast was visible for about 5 minutes. The explosion had also been slightly obscured to the crew at Johnston Island by cloud coverage. The blast from Orange did not cause the large communication interruption that Teak had caused, but some commercial flights to Hawaii were said to have lost contact with air traffic controllers for a short period of time.[4]^:271

Operation Hardtack I Cactus shot Crater on Runit Island

The Cactus test took place May 6, 1958 at approximately 0615. An 18 Kiloton land-surface type shot was detonated on a platform at the northern tip of Runit, Enewetak in the second of the 35 tests for Operation Hardtack I.[4]^:2The initial cloud from the explosion reached as high as 19,000 feet (5.79 km) within the first ten minutes, and settled at around 15,000 feet (4.57 km) by 20 minutes after detonation. The nuclear fallout prediction map proved to be accurate in determining the span and the intensity of the resultant fallout.[4]^:149–87Measured peak intensity of fallout reached 440 R at hour three directly above blast site on the North end of the Atoll. At mid-island the radiation was measured to be 1.7 R. The southern tip received a very small amount of radiation, 0.005 R due to the easterly winds.

Out of the eight Programs listed, DOD-affiliated Projects 1.4, 1.7, 1.8, 1.9, 1.12, 2.8, 3.2, 5.2, 5.3, 6.4, 6.5 and 6.6 involved the Cactus test.[4]^:149–87

One of the goals of this test was to study the physical characteristics of the crater and the surrounding area pre- and post-detonation associated with Project 1.4. A camera was mounted to a RB-50 aircraft and the resultant crater was mapped using photogrammetry. Measurements were taken from 500 feet (152 m) down to ground zero for both pre- and post detonation. Survey measurements of the Cactus test could not be made until the resultant radiation amounts had lowered to safer levels.[4]^:114–38 Along with photogrammetric radial measurements, Airblast measurements were also recorded near surface zero for Cactus in accordance with Project 1.7. Similar to Project 1.8, Project 1.9 sought to determine transmission of blast pressure through the ground soil. Forty-three drums were buried at varying depths 600 feet (183 meters) from ground zero of the Cactus detonation. Individuals from the Air Force Ballistic Missile Division – TRW Space Technologies Laboratory sought to the Shock Spectra Studies of Project 1.12. Measurement gauges were located between 625 and 965 feet (191 and 294 m) from the blast site. Fallout measurements and samples were taken by aircraft in the aftermath of the detonation, as part of Project 2.8. These surveys were designed in part to determine the impact of specific radionuclides to overall nuclear fallout. Samples were taken early post-blast using a new rocket sampler, the UCRL, which were then followed by B-57D and WB-50 aircraft. Between four and twenty-four hours post-detonation, the WB-50 collected several samples at 1,000 feet (300 m) in altitude. Project 3.2 involved structural tests of corrugated steel arches. One of these arches was placed 980 feet (299 meters) away from the Cactus blast site. Eight days after the test, a crew of 13 men were allowed near the surface zero in order to extract the arch. The extraction took around twelve hours, and the radioactivity levels reached a maximum at 0.420 R/h during this time. Project 5.2 sought to determine the effects of the blast on two A4D-1 aircraft, both in thermal radiation and pressure. Nine film badges were placed throughout each aircraft in order to measure radiation. The Gamma dosimeter worn by the pilot in aircraft 827 indicated a neutron exposure level of 0.105 rem. There is not information available for the dosimeter worn by the pilot in aircraft 831. Radiation recorded by six of the nine film badges ranged from 0.49-1.74R. Information from the remaining three film badges, located at the Pilot's right leg, left sleeve, and left vest is not available. The pilot's exposures were both greater than 3R. Project 5.3 was very similar to 5.2, focusing on the effects of the blast on the structure of two test FJ-4 aircraft. Radiation from film badges on aircraft 467 ranged from 0.52-3.71 R, and 1.23-5.06 R for aircraft number 310. In Project 6.4, the Army Signal Research and Development Laboratory (SRDL) investigated the electromagnetic pulses post-detonation, utilizing two instruments, one at Wotho (roughly 240 nautical miles from Enewetak) and one at Kusaie (around 440 nautical miles from Enewetak). Though Cactus is mentioned in Project 6.5, whose goal was to study the radar echoes from the fireball, it is not clear what destroyers were involved if any. Destroyers for the Teak, Fir and Yucca tests are explicitly stated. Project 6.6, the lasts of the projects that involved the Cactus test, sought to measure the physical properties of the stabilized radioactive cloud following the blast.[4]^:114–38

At 0630 on May 13, the Koa surface device was detonated at the western side of Dridrilbwij. The size of the blast was 1.37 MT, around 76 times larger than the yield of the previous surface test, Cactus. The test was conducted in a large water tank. Within 17 minutes of the blast, surface clouds reached approximately 60,000 feet (18 km). Nuclear fallout predictions for Koa were larger and covered a broader range than Cactus, with significantly higher radiation levels, an order of magnitude larger, in the immediate region surrounding the blast.[4]^:44 There had been a larger nuclear barge detonation, the 1.85 MT Apache test, off the island of Dridrilbwij two years prior in 1956, during which the island survived.[7] The detonation of the Koa device, however, caused complete destruction of the island.[4]^:44

The Department of Defense (DOD) sponsored a series of experiments for Koa: Projects 1.4, 1.7, 1.8, 1.9, 1.12, 2.9, 3.2, 3.6, 5.1, 5.3. 6.4, 6.5, 6.6, 6.9. and 6.11.[4]^:149–87 Project 1.4, which sought to study land craters post detonation for several shots, took ground survey measurements from surface zero out to 2,500 feet (760 m). Detailed measurements could not be made until four days after the blast due to radiation levels. Using a boat, the majority of the crater was mapped, though some measurements could not be made until 1959 due to radioactivity levels around the Koa blast site. In Project 1.9, the blast-induced pressure through the soil was measured by burying 43 drums at depths ranging from 0 to 20 feet and around 3,000 feet (910 m) feet from the Koa blast site. The early radioactive cloud samples, normally collected post-shot as a part of Project 2.8 using a UCRL rocket sampler, were not collected after the Koa test due to technical difficulties. Fallout at high and low altitudes utilizing B-57D and WB-50 aircraft were measured with no technical problems. Project 3.6, which was conducted only on Koa, tested the effects of the blast on reinforced-concrete slabs buried close to surface zero. One station was located at 1,830 feet (560 m) from the blast site, and the other was located 3,100 feet (940 m) away. Project 5.2 was designed to measure the radiation levels using film badges on different areas of the aircraft and on the pilot directly. Koa had the lowest average radiation measurements of the eight shots on this project, with aircraft 827 ranging from 0.01-0.02R and aircraft 831 reporting levels between 0.03-0.19R. Unlike in the Cactus test, all nine film badges from both aircraft were successfully recovered and reported.[4]^:114–38

Quince and Fig were a series of surface shots that occurred in early August at the center of Runit. They were the last of the Hardtack tests conducted at the Enewetak Atoll. Quince was detonated at 2:15pm on August 6, 1958. Twelve days later, the Fig device was detonated on August 18, 1958 at 4:00pm. Quince and Fig were UCRL devices with co-sponsorship through the DOD and the AEC, though the main focus of these tests was weapons development. One of the main differences between these two tests was that over 130 tons of soil from the Nevada Test Site had been shipped in and was placed at surface zero of the Fig test. The radioactive cloud from the Quince blast rose to 1,500 feet (460 m). As Runit was to also be the detonation site for Fig, the area had to be decontaminated after the Quince test. Around three to five inches of contaminated topsoil was removed from an area 75 feet by 25 feet upwind of ground zero. An area of 60 square feet at the blast site was scraped to remove the top three inches of soil as well. Even with these precautions, the measured alpha activity was around 20,000 counts per minute (CPM), and the area closest to surface zero was roped off to prevent personnel from entering. Upon detonation, the mushroom cloud produced by the Fig device rose to approximately 6,000 feet (1.8 km), with a base of roughly 4,300 feet (1.3 km). 30 minutes post detonation, radiation measurements at the blast site reached over 10,000 R/hr.[4]^:219–22

The DOD experiments for Quince and Fig included Projects 1.4, 1.7. 2.4, 2.9, 2.10, 2.11, 2.14. and 8.7.[4]^:219–22

FIR predicted fallout, surface radiological exclusion (radex) areas, ship position, and aircraft participation. FIR was the first Bikini detonation of the Hardtack series. Detonated at 0550 on May 12, 1958. FIR was detonated on a barge in the BRAVO crater, producing a 1.36 Mt yield range.[3] After detonation, the cloud rose to 60,000 to 90,000 feet (18.3–27.4 km). The FIR detonation was shortly followed by BUTTERNUT detonation on Enewetak 25 minutes later. DOD-sponsored experiments for FIR included Projects 3.7, 5.1, 6.4, 6.5, 6.6 and 6.11.[3]^:2[4]^:152

BUTTERNUT predicted fallout, surface radiological exclusion areas (radex), ship positions, and aircraft participation. Butternut was detonated at 0615 on May 12, 1958, 25 minutes after FIR had been detonated at Enewetak. BUTTERNUT was detonated on a barge 4,000 feet (1.22 km) west of Runit, producing a yield range of 81 kt.[3] The cloud rose to 35,000 feet (11 km), stabilizing at 30,000 feet (9.1 km). The DOD-sponsored experiments for BUTTERNUT were Projects 5.1, 5.2, 5.3, 6.5, 6.6, and 6.9.[3]^:2[4]^:152

HOLLY predicted fallout, surface radiological exclusion (radex) areas, ship positions, and aircraft participation. HOLLY was detonated at 0630 on May 21, 1958 on a barge west of Runit, 4,000 feet (1.22 km) from the nearest edge of the island, producing a 5.9 kt yield range.[3] The detonation produced a 15,000 feet (4.6 km) cloud that stabilized at an altitude of 12,000 feet (3.7 km) at the top and 7,500 feet (2.3 km) at its base. Project 6.6, was the only DOD-sponsored experiment for HOLLY, and was conducted on Enewetak Island.[3]^:2[4]^:192

NUTMEG predicted fallout, surface radiological exclusion area (radex), ship positions, and aircraft participation. The second Bikini shot, NUTMEG, was detonated at 0920 on May 22, 1958. NUTMEG was detonated on a barge in the ZUNI crater, and produced a 25.1 kt yield range.[3] The detonation cloud stabilized at 20,000 feet (6.1 km) by 0926. DOD-sponsored experiments for NUTMEG were Projects 6.3, 6.3a, 6.4, 6.5, 6.6, and 6.11. Projects 6.3 and 6.3a had stations near the burst point on Eneman Island.[3]^:2[4]^:156

YELLOWWOOD predicted fallout, surface radiological (radix) exclusion area, and ship positions. YELLOWWOOD was detonated at 1400 on May 26, 1958. YELLOWWOOD was detonated on a barge 5,000 feet (1.5 km) southwest of Enjebi, and produced a 330 kt yield range.[3] The DOD sponsored 13 experiments for YELLOWWOOD: Projects 2.4, 2.8, 3.7, 5.1, 5.2, 5.3, 6.4, 6.5, 6.6, 6.8, 6.9, 6.11, and 8.1. Instrument stations for Project 2.4 were located on buoys in the lagoon. The remaining projects had more distant stations or were primarily airborne.[3]^:2[4]^:193–5

Predicted fallout, surface radiological exclusion (radix) area, ship positions, and aircraft participation. MAGNOLIA was detonated at 0600 on May 27, 1958. MAGONLIA was detonated on a barge 3,000 feet (914 m) southwest of the center of Runit, and produced a 57 kt yield range.[3] The detonation produced a 44,000-foot (13.4 km) cloud that stabilized at 41,000 feet (12.5 km) with its base at 15,000 feet (4.6 km). The DOD-sponsored experiments for MAGNOLIA were Projects: 3.7, 5.2, and 5.3. Instruments for Project 3.7 were on Boken, Enjebi, and Runit.[3]^:2[4]^:197

TOBACCO predicted fallout, surface radiological exclusion (radix) area, ship positions, and aircraft participation. TOBACCO was detonated at 1415 on May 30, 1958. TOBACCO was detonated on a barge 3,000 feet (914 m) northwest of Enjebi, and produced an 11.6 kt yield range.[3] The detonation produced an 18,000-foot (5.5 km) cloud that stabilized at 16,000 feet (4.9 km) by 1430. The DOD-sponsored experiments for TOBACCO were Projects 3.7, 5.1, 5.2, 5.3, and 6.8. The project activity for Project 3.7 was on Boken, Enjebi, and Runit. Project 6.8 simply monitored TOBACCO from stations off Enewetak and Parry islands.[3]^:2[4]^:199

SYCAMORE predicted fallout, surface radiological exclusion (radex) area, ship positions, and aircraft participation. SYCAMORE was detonated at 1500 on May 31, 1958. SYCAMORE was detonated on a barge moored in the BRAVO crater, and produced a 92 kt yield range.[3] DOD-sponsored experiments for SYCAMORE were Projects: 3.7, 5.1, 6.4, 6.5, 6.6, and 6.11. Only Project 6.11 had an instrument site at the Bikini Atoll.[3]^:2[4]^:160

MAPLE predicted fallout, surface radiological exclusion (radex) area, ship positions, and aircraft participation. MAPLE was detonated on June 11 at 0530 1958. MAPLE was detonated on a barge just south of Lomilik, and produced a 213 kt yield range.[3] The 40,000 feet (12.2 km) cloud produced by the detonation was tracked by radar from Benner. The DOD-sponsored experiments for MAPLE were Projects 5.1, 6.3, and 6.3a. Projects 6.3 and 6.3a shared the same, rather close-in sites on Lomilik.[3]^:2[4]^:162

ASPEN predicted fallout, surface radiological exclusion (radex) areas, ship positions, and aircraft participation. ASPEN was detonated on 15 June 58 at 0530. ASPEN was detonated on a barge in the BRAVO crater of Bikini, 4,000 ft (1.22 km) southwest of Nam. ASPEN produced a 319 kt yield range.[3] The detonation produced a 48,600-foot (14.8 km) cloud as measured by radar from Benner. No experiments were sponsored by the DOD for this shot.[3]^:2[4]^:154

WALNUT predicted fallout, surface radiological exclusion (radex) areas, ship positions, and aircraft participation. WALNUT was detonated on June 15, 1958 at 0630, 1 hour after the ASPEN event at Bikini. WALNUT was detonated on a barge 5,000 feet (1.52 km) southwest of Enjebi Island in Enewetak. The detonation produced a 61,000 feet (18.6 km) cloud, and produced a 1.45 Mt yield range.[3] The DOD-sponsored experiments for WALNUT included Projects 2.4, 2.8, 3.7, 5.1, 5.2, 5.3, and 8.1.[3]^:2[4]^:154

LINDEN predicted fallout, surface radiological exclusion (radex) area, ship positions, and aircraft participation. LINDEN was detonated on June 18, 1958 at 1500. LINDEN was detonated on a barge 4,000 ft (1.22 km) west of the center of Runit Island at Enewetak. The detonation produced a 20,000-foot (6.1 km) cloud with a 7,000-foot (2.1 km) base, and produced an 11 kt yield range.[3] No DOD-sponsored experiments were conducted during LINDEN.[3]^:2[4]^:203

REDWOOD predicted fallout, surface radiological exclusion (radex) areas, ship positions, and aircraft participation. REDWOOD was detonated on June 28, 1958 at 0530. REDWOOD was detonated on a barge south of Lomilik in Bikini. REDWOOD was followed by the ELDER detonation at Enewetak Atoll one hour later. The detonation cloud base was at 28,000 feet (8.5 km) and the top stabilized at 55,000 feet (16.8 km), and produced a 412 kt yield range.[3] The only DOD-sponsored experiment for REDWOOD was Project 5.1.[3]^:2[4]^:168

ELDER predicted fallout, surface radiological exclusion (radex) areas, ship positions, and aircraft participation. ELDER, detonated on June 28, 1958 at 0630. ELDER was the second of a tandem shot with REDWOOD (detonated an hour earlier on Bikini). ELDER was detonated on a barge 1 nmi (1.85 km) southeast of Enjebi Island in Enewetak. Initial cloud height had been well over 65,000 feet (19.8 km), and produced an 880 kt yield range.[3] The only DOD-sponsored experiment for ELDER was project 5.1.[3]^:2[4]^:168

OAK predicted fallout, surface radiological exclusion (radex) area, and ship positions. OAK, one of the largest detonations at Enewetak Atoll, and was fired at 0730 on June 29, 1958. OAK was detonated on a barge moored on the reef 21,000 feet (6.40 km) southwest of Bokoluo Island. It was followed at noon by the HICKORY shot at Bikini. The Initial height of the cloud was estimated to be 78,000 feet (23.8 km), and produced an 8.9 MT yield range.[3] Two DOD-sponsored experiments were included for OAK: Projects 2.8 and 5.1.[3]^:2[4]^:205

HICKORY predicted fallout, surface radiological exclusion (radex) area, ship positions, and aircraft participation. HICKORY was detonated on June 29, 1958 at 1200. HICKORY was detonated on a barge off the west end of Enema at Bikini, 4½ hours after the OAK shot at Enewetak Atoll. The detonation cloud rose to 24,200 feet (7.4 km) with an estimated 12,000-foot (3.7 km) base, and produced a 14 kt yield range.[3] Projects 6.3 and 6.3a were the only DOD-sponsored experiments for HICKORY.[3]^:2[4]^:170

SEQUOIA predicted fallout, surface radiological exclusion (radex) area, ship positions, and aircraft participation. SEQUOIA was detonated on July 2, 1958 at 0630. SEQUOIA was detonated on a barge 2,000 feet (610 m) west-northwest of Runit Island at Enewetak. The cloud stabilized at 15,000 feet (4.57 km), and produced a 52 kt yield range.[3] SEQUIA had no DOD-sponsored experiments.[3]^:2[4]^:209

CEDAR predicted fallout, surface radiological exclusion (radex) area, ship positions, and aircraft participation. CEDAR was detonated on July 3, 1958 at 0530. CEDAR was detonated on a barge in the BRAVO crater southwest of Nam, 4,000 feet (1.2 km) from the edge of the island at Bikini. The CEDAR detonation produced a 50,000-foot (15.2 km) cloud, and produced a 220 kt yield range.[3] The only DOD-sponsored experiment for CEDAR was Project 5.1.[3]^:2[4]^:172

DOGWOOD predicted fallout, surface radiological exclusion (radex) area, ship positions, and aircraft participation. DOGWOOD was detonated on July 6, 1958 at 0630. DOGWOOD was detonated on a barge southwest of Enjebi, 4,000 feet (1.22 km) from the edge of the island at Enewetak. The cloud rose to 58,000 feet (17.7 km), stabilizing at 54,000 feet (16.5 km) with a 35,000-foot (10.7 km) base, and produced a 397 kt yield range.[3] The only DOD-sponsored experiment for DOGWOOD Was Project 5.1.[3]^:2[4]^:211

POPLAR predicted fallout, surface radiological exclusion (radex) area, ship positions, and aircraft participation. POPLAR was detonated on July 12, 1958 at 1530. POPLAR was detonated on a barge southwest of Nam, at Bikini. The detonation cloud quickly rose above the tracking radar limits of 61,000 feet (18.6 km), and the base was established at 42,000 feet (12.8 km) at 1540, and produced a 9300 kt yield range.[3] The only DOD-sponsored experiment for POPLAR was Project 3.7.[3]^:2[4]^:176

SCAEVOLA predicted fallout, surface radiological exclusion (radex) area, ship positions, and aircraft participation. Scaevola was detonated on July 14, 1958 at 1600. Scaevola was detonated on a barge west of Runit Island at Enewetak. Its yield was low and the explosion did not destroy the shot barge but only damaged it, producing a 0 kt yield range.[3] No DOD-sponsored experiments were scheduled for Scaevola.[3]^:2[4]^:213

PISONIA predicted fallout, surface radiological exclusion (radex) area, ship positions, and aircraft participation. PISONIA was detonated on July 18, 1958 at 1100. PISONIA was detonated on a barge 10,000 feet (3.05 km) west of Runit Island at Enewetak. The cloud rose immediately to 55,000 feet (16.8 km), and produced a 255 kt yield range.[3] No DOD-sponsored experiments were scheduled for PISONIA.[3]^:2[4]^:215

JUNIPER predicted fallout, surface radiological exclusion (radex) area, ship positions, and aircraft participation. JUNIPER, the last nuclear detonation to occur at Bikini, was detonated on July 22, 1958 at 1620. JUNIPER was detonated on a barge 4,000 feet (1.22 km) from the west end of Eneman in the ZUINI crater at Bikini . The detonation cloud rose to 40,000 feet (12.2 km) with an estimated 24,000-foot (7.32 km) base, and produced a 65 kt yield range.[3] No DOD-sponsored experiments were scheduled for JUNIPER.[3]^:2[4]^:180

OLIVE predicted fallout, surface radiological exclusion (radex) area, ship positions, and aircraft participation. OLIVE was detonated on July 23, 1958 at 0830. OLIVE was detonated on a barge southwest of Enjebi Island, at Enewetak Atoll. 4,000 feet (1.22 km) from the nearest land at Enewetak. The cloud rose to 50,000 feet (15.2 km) with an estimated 15,000-foot (4.57 km) base, and produced a 202 kt yield range.[3] No DOD-sponsored experiments were scheduled for OLIVE.[3]^:2[4]^:217

PINE predicted fallout, surface radiological exclusion (radex) area, ship positions, and aircraft participation. PINE was detonated on July 27, 1958 at 0830. PINE was detonated on a barge southwest of Enjebi Island, 8,500 feet (2.59 km) from the nearest land, at Enewetak. The cloud rose quickly to 66,000 feet (20.1 km) with an estimated 38,000-foot (11.6 km) base as measured by radar, and produced a 2 Mt yield range.[3] No DOD-sponsored experiments were scheduled for PINE.[3]^:3[4]^:220

Another reason for underwater tests was to detect radiation contamination of ships after an underwater nuclear explosion. This meant that the contaminated ships required unique "radsafe" preparations so that the data could be quickly accounted for. After the data on the damage and radiation was recorded, the ships needed decontamination work completed before repairs could be completed. The Radiological and Decontamination Unit consisting of 200 enlisted and one officer was created for the task of decontamination.[4]^:70–86 After decontamination, the target ships were repaired for use in a second underwater nuclear weapons test. The amount of radiation exposure was debated for the safety of the crews. Roentgens (1 R = ca 0,01 Gy in soft tissue) were used to gauge the gamma radiation that affected the units working on the nuclear tests.

For the underwater test crew, a limit of 5 R per blast along with 10 R per operation was referenced as the limit for exposure. These initial limits were rejected and maximum permissible exposure standards (MPE) were solidified by commanders for the crews working on the decontamination unit. Due to the fast recovery of ships, high contamination values were expected by commanders and set the standard to four roentgens per hour (R/hr). An excess of 4 R/hr was designated off limits of recovery units. Personnel were given special breathing equipment to work in the interior of ships with an R/hr higher than one. High numbers of personnel working the tests were used to keep individuals within the MPE. Times were calculated to keep the total exposure below two roentgens for the personnel working on the ships. A floating decontamination facility was created on board a transport ship for the Wahoo and Umbrella nuclear tests. This allowed important data analysis and an increase in recovery efficiency.[4]^:70–86

The nuclear explosion was carried out in open ocean outside of Enewetak. This nuclear test codenamed Wahoo was the first underwater test in the Operation Hardtack series. This test could be considered a continuation of the Wigwam nuclear blast (a deep water nuclear test 500 nautical miles (930 km; 580 mi) off the coast of San Diego).[8] Like its predecessor, the Wahoo shot was a scientific program that studied the effects of an underwater nuclear blast on Navy systems. The nuclear device was positioned 500 feet (150 m) deep in the Pacific Ocean. This deep water test required precise targeting arrays to be set up around the blast location, which presented unique problems for the arrays as the winds, sea currents and tides needed to be within certain limits for the data to be accurate. Testing arrays were placed at depths of 400 to 800 fathoms (2400 to 4800 feet, 732 to 1463 meters) around the nuclear device. The deep water mooring systems needed for the test proved to be difficult to position, leading many analysts to believe the data skewed. The target ships to be used for this program consisted of three destroyers, an active submarine, a submarine mockup used in Wigwam tests, and a merchant marine ship.[4]^:225 It was predicted that no air blast or thermal effects would be presented from the underwater blast. The fallout from the blast was also predicted to stay within the target array due to the southwest surface winds.

The test conditions were met on May 16 allowing for the nuclear device to be detonated. Within a second of detonation, a spray dome was created that reached a height of 840 feet (260 m) after seven seconds. The overall shape of the spray dome resembled a cone with 45 degree sloped sides. Plumes were seen breaking through the spray dome after six seconds in every direction. The vertical plume continued rising until 12 seconds after the blast while the lateral plumes traveled for 20 seconds before collapsing. The diameter of the spray dome was approximately 3,800 feet (1,200 m) at the 20 second mark.[4]^:237 The base surge reached a radius of 8,000 feet (2,400 m) in the downwind direction after 1.7 seconds. The downwind surge aided by a 15 knot wind reached speeds of 21 knots (24.2 mph). This base surge could be seen for three and a half minutes and for longer from the air as it continued to move across the ocean. When the spray dome and base surge had dissipated, a foam patch could be seen spreading from the surface zero water to reach over 6,000 feet (1,800 m).[4]^:238 The nuclear blast was calculated to be nine kilotons. All fallout stayed within the predicted fallout area with a maximum of 0.030 R/hr. The target ship at 5,900 yards (5,400 m) was directly hit by the shockwave, vibrating the entire ship and shaking it violently. The Moran merchant marine ship moored at 2,346 feet (715 m) away was immobilized due to shock damage to its main and auxiliary equipment while also suffering minor hull damage. One hour and ten minutes after detonation, a five-gallon water sample was taken directly above the blast location showing 5 R/hr. The retrieval team entered a 3.8 R/hr field after an hour and thirty five minutes.

The second underwater explosion of the Operation Hardtack series was code-named Umbrella. This test was conducted in the lagoon inside Enewetak. This test could be considered a continuation of underwater test Baker, which was conducted in Bikini Lagoon. Explosions in shallow water can create an underwater crater if close enough to the bottom. The target ships from the Wahoo test were towed into the lagoon to be used again for the Umbrella test. The damage from Wahoo was minor in all cases with the exception of the Moran which required extra refurbishing of the hull. These ships had to be washed down and have the measuring equipment replaced before being put into use. The mooring for Umbrella was considerably easier than for Wahoo due to the location and depth of the lagoon. Information gathered from the Wahoo shot directly affected the Umbrella plans with regard to target array placement and decontamination times. The device was placed with a buoy at a depth of 150 feet (46 m).[8]

June 9 saw the second underwater nuclear test of the Hardtack I series. The detonation occurred at 11:15 AM (local time) with clear skies and a 15 to 17-knot wind from the east-northeast. Within one-tenth of a second, the spray dome had broken through the surface. The overall shape of the spray dome resembled a vertical column with the plumes helping create the shape. Within 20 seconds of detonation, the maximum height of the column reached 5,000 feet (1,500 m). The base surge reached a distance around 10,000 feet (3,000 m) downwind, reaching out approximately 6,000 feet (1,800 m) in all directions. This base surge could be seen from the air for about 25 minutes and the foam patch over the blast location lasting even longer.[4]^:248 The blast yield of the nuclear device was measured to be eight kilotons. The Umbrella blast created a crater 3,000 ft (910 m) in diameter and 20 ft (6.1 m) in depth in the lagoon. The maximum radiation reading was found to be 0.350 R/hr by an aircraft flying over the blast location. Radiation was reported to be of small portions, and re-entry was granted 30 minutes after detonation. Out of the major target ships, the highest radiation reading was logged at 0.0015 R/hr of the stern of the Moran. After all scientific data had been gathered from the target ships, they were restored to be seaworthy and towed back to Pearl Harbor. The Moran was concluded to be unseaworthy due to the blast and was sunk by naval gunfire near Ikuren Island.[4]^:251

The underwater nuclear tests (Wahoo and Umbrella) gathered scientific data that helped the Department of Defense understand the effects of nuclear weapons on Navy ships. Some of the key points found were that underwater nuclear blasts create less fallout due to the absorption of radioactive material in the water and vaporized droplets. Direct gamma radiation was found to be extremely low, but the base surge was found to be highly radioactive as it passed measurement devices. Smaller radiation concentrations followed in waves mimicking the initial base surge. Almost all free-field radiation activity was found to disappear after fifteen minutes allowing for return to normal operations.[6]^:86 The impact of shock waves was less than previously expected. The damage from the shockwave was found to be negligible on the destroyers at the ranges tested, but equipment failure from the blast could immobilize the ships. The preliminary tests of explosive tapered charges were proven to simulate the shock waves of a nuclear device according to the data gathered.[6]^:91