Academic literature on the topic 'White Sands Dune Field'
Create a spot-on reference in APA, MLA, Chicago, Harvard, and other styles
Consult the lists of relevant articles, books, theses, conference reports, and other scholarly sources on the topic 'White Sands Dune Field.'
Next to every source in the list of references, there is an 'Add to bibliography' button. Press on it, and we will generate automatically the bibliographic reference to the chosen work in the citation style you need: APA, MLA, Harvard, Chicago, Vancouver, etc.
You can also download the full text of the academic publication as pdf and read online its abstract whenever available in the metadata.
Journal articles on the topic "White Sands Dune Field"
1
Rachal, David M., and Daniel P. Dugas. "Historical Dune Pattern Dynamics: White Sands Dune Field, New Mexico." Physical Geography 30, no. 1 (2009): 64–78. http://dx.doi.org/10.2747/0272-3646.30.1.64.
Full text
2
Zhao, Feifei, Benjamin T. Cardenas, and Wonsuck Kim. "Controls of aeolian dune height on cross-strata architecture: White Sands Dune Field, New Mexico, U.S.A." Journal of Sedimentary Research 91, no. 5 (2021): 495–506. http://dx.doi.org/10.2110/jsr.2020.138.
Full textAbstract:
ABSTRACT The stratal types composing aeolian dunes preserve a record of the transport and sorting of grains and are categorized into: 1) grainflow strata, 2) grainfall laminae, and 3) wind-ripple laminae. The arrangement of these deposits in the cross beds of a formative dune is largely unexplored. Here, field results from White Sands Dune Field, New Mexico, USA, are used to test the hypothesis that dune height controls the arrangement, abundance, and geometry of cross-stratification types. Grainflow thicknesses and deposit widths were measured on wind-scoured stoss-side exposures of seven crescentic dunes with heights ranging from 1.7 m to 11.2 m. Dozens of grainflow thickness measurements were taken along transverse-oriented strata normal to the crest on each dune. The results show that grainflow thickness averages from 1 cm to 4 cm. These data show a positive trend between mean grainflow thickness and dune height but only for the grainflow thicknesses measured at the bases of dunes. The tallest dune (11.2 m) produced many thick grainflow packages of 10 cm to 30 cm in which individual grainflow strata were indistinguishable from each other. This amalgamation was also found to be characteristic of larger dunes—the product of a lack of grainfall deposits separating individual grainflows. These differences in grainflow strata at the bases of dune lee slopes are linked to the temporary storage of sediment along the upper parts of lee slopes. In taller dunes with longer lee slopes, amalgamated grainflows which require multiple avalanche events and take longer time to reach the base transport temporarily stored sediment at upper parts of the slope. This allows time for wind ripples to rework accumulations near the base, where grainfall deposition is also limited. Shorter dunes lack this temporary storage mechanism, as individual grainflows can move across the entire lee slope in a single event, and grainfall accumulates across the entire lee slope. These stratigraphic measurements and process-based understanding will be useful in estimating original dune height in ancient cross-strata and will lead to a better interpretation of aeolian stratigraphy.
3
Kocurek, Gary, Mary Carr, Ryan Ewing, Karen G. Havholm, Y. C. Nagar, and A. K. Singhvi. "White Sands Dune Field, New Mexico: Age, dune dynamics and recent accumulations." Sedimentary Geology 197, no. 3-4 (2007): 313–31. http://dx.doi.org/10.1016/j.sedgeo.2006.10.006.
Full text
4
Brothers, Sarah C., Gary Kocurek, Thomas C. Brothers, and Ilya V. Buynevich. "Stratigraphic architecture resulting from dune interactions: White Sands Dune Field, New Mexico." Sedimentology 64, no. 3 (2016): 686–713. http://dx.doi.org/10.1111/sed.12320.
Full text
5
Pedersen, Anine, Gary Kocurek, David Mohrig, and Virginia Smith. "Dune deformation in a multi-directional wind regime: White Sands Dune Field, New Mexico." Earth Surface Processes and Landforms 40, no. 7 (2015): 925–41. http://dx.doi.org/10.1002/esp.3700.
Full text
6
Dong, Pinliang, Jisheng Xia, Ruofei Zhong, Zhifang Zhao, and Shucheng Tan. "A New Method for Automated Measurement of Sand Dune Migration Based on Multi-Temporal LiDAR-Derived Digital Elevation Models." Remote Sensing 13, no. 16 (2021): 3084. http://dx.doi.org/10.3390/rs13163084.
Full textAbstract:
While remote sensing methods have long been used for coastal and desert sand dune studies, few methods have been developed for the automated measurement of dune migration in large dune fields. To overcome a major limitation of an existing method named “pairs of source and target points (PSTP)”, this paper proposes a toe line tracking (TLT) method for the automated measurement of dune migration rate and direction using multi-temporal digital elevation models (DEM) derived from light detection and ranging (LiDAR) data. Based on a few simple parameters, the TLT method automatically extracts the base level of a dune field and toe lines of individual dunes. The toe line polygons derived from two DEMs are processed using logical operators and other spatial analysis methods implemented in the Python programming language in a geographic information system. By generating thousands of random sampling points along source toe lines, dune migration distances and directions are calculated and saved with the sampling point feature class. The application of the TLT method was demonstrated using multi-temporal LiDAR-derived DEMs for a 9 km by 2.4 km area in the White Sands Dune Field in New Mexico (USA). Dune migration distances and directions for three periods (24 January 2009–26 September 2009, 26 September 2009–6 June 2010, and 24 January 2009–6 January 2010) were calculated. Sensitivity analyses were carried out using different window sizes and toe heights. The results suggest that both PSTP and TLT produce similar sand dune migration rates and directions, but TLT is a more generic method that works for dunes with or without slipfaces that reach the angle of repose.
7
Baitis, Elke, Gary Kocurek, Virginia Smith, David Mohrig, Ryan C. Ewing, and A. P. B. Peyret. "Definition and origin of the dune-field pattern at White Sands, New Mexico." Aeolian Research 15 (December 2014): 269–87. http://dx.doi.org/10.1016/j.aeolia.2014.06.004.
Full text
8
Pelletier, Jon D. "Controls on the large-scale spatial variations of dune field properties in the barchanoid portion of White Sands dune field, New Mexico." Journal of Geophysical Research: Earth Surface 120, no. 3 (2015): 453–73. http://dx.doi.org/10.1002/2014jf003314.
Full text
9
Langford, Richard P. "The Holocene history of the White Sands dune field and influences on eolian deflation and playa lakes." Quaternary International 104, no. 1 (2003): 31–39. http://dx.doi.org/10.1016/s1040-6182(02)00133-7.
Full text
10
Phillips, J. D., R. C. Ewing, R. Bowling, et al. "Low-angle eolian deposits formed by protodune migration, and insights into slipface development at White Sands Dune Field, New Mexico." Aeolian Research 36 (February 2019): 9–26. http://dx.doi.org/10.1016/j.aeolia.2018.10.004.
Full textDissertations / Theses on the topic "White Sands Dune Field"
1
Johnson, Jeffrey R., Cherie Achilles, James F. Bell, et al. "Visible/near-infrared spectral diversity from in situ observations of the Bagnold Dune Field sands in Gale Crater, Mars." AMER GEOPHYSICAL UNION, 2017. http://hdl.handle.net/10150/626566.
Full textAbstract:
As part of the Bagnold Dune campaign conducted by Mars Science Laboratory rover Curiosity, visible/near-infrared reflectance spectra of dune sands were acquired using Mast Camera (Mastcam) multispectral imaging (445-1013nm) and Chemistry and Camera (ChemCam) passive point spectroscopy (400-840nm). By comparing spectra from pristine and rover-disturbed ripple crests and troughs within the dune field, and through analysis of sieved grain size fractions, constraints on mineral segregation from grain sorting could be determined. In general, the dune areas exhibited low relative reflectance, a weak similar to 530nm absorption band, an absorption band near 620nm, and a spectral downturn after similar to 685nm consistent with olivine-bearing sands. The finest grain size fractions occurred within ripple troughs and in the subsurface and typically exhibited the strongest similar to 530nm bands, highest relative reflectances, and weakest red/near-infrared ratios, consistent with a combination of crystalline and amorphous ferric materials. Coarser-grained samples were the darkest and bluest and exhibited weaker similar to 530nm bands, lower relative reflectances, and stronger downturns in the near-infrared, consistent with greater proportions of mafic minerals such as olivine and pyroxene. These grains were typically segregated along ripple crests and among the upper surfaces of grain flows in disturbed sands. Sieved dune sands exhibited progressive decreases in reflectance with increasing grain size, as observed in laboratory spectra of olivine size separates. The continuum of spectral features observed between the coarse- and fine-grained dune sands suggests that mafic grains, ferric materials, and air fall dust mix in variable proportions depending on aeolian activity and grain sorting.
2
Baitis, Elke Elise. "Patterns and paleoshorelines of White Sands Dune Field, New Mexico." Thesis, 2011. http://hdl.handle.net/2152/ETD-UT-2011-05-3354.
Full textAbstract:
The dune field at White Sands, New Mexico, shows a well-defined pattern of dunes and interdune areas, as well as spatial variations in this pattern. The purpose of this research is to determine which measured pattern parameters are most consistent across the dune field and to determine the cause of depositional spatial variability. This was accomplished using an airborne LiDAR generated digital-elevation model (DEM) collected in June 2007 and covering 39 km² of the dune field. Properties of the dune field are defined by measurements from three dune populations: 1) 110 randomly selected dunes, 2) 247 dunes along transects oriented in the net transport direction, and 3) 171 dunes from three zones within the field where differences in pattern are visible. Measurements of eight common dune parameters show that the lowest coefficients of variation occur with dune orientation and crestline sinuosity, which largely define the field pattern. Cross-plotting of parameters shows generally poor correlations, which is thought to reflect variation around field-scale means that are comparable to other dune fields globally. Removing the dunes from the LiDAR DEM reveals a depositional substrate with breaks in slope interpreted as three paleoshorelines associated with Pleistocene Lake Otero. The paleoshorelines are antecedent boundary conditions that exert the primary control on spatial variability within the dune pattern.<br>text
3
Pederson, Anine Oehlenschlaeger. "Dune behavior in a multidirectional wind regime : White Sands Dune Field, New Mexico." Thesis, 2014. http://hdl.handle.net/2152/26917.
Full textAbstract:
As with most dune fields, the White Sands Dune Field in New Mexico forms in a wind regime that is not unimodal. In this study, dune behavior at White Sands was documented from a time series of five lidar-derived digital elevation models (DEM) and compared to a record of wind direction and speed during the same period. For the study period of June 2007 - June 2010, 244 sand-transporting wind events occurred and define a dominant wind mode from the SW and lesser modes from the NNW and SSE. Based upon difference maps and tracing of dune brinklines, overall dune behavior consists of migration to the NE, but with along-crest migration of dune sinuosity to the SE. Permutations of the DEMs allow matching specific dune behavior with wind modes. The SW winds are transverse to dune orientations and cause most forward migration. The NNW winds cause along-crest migration of dune sinuosity and low stoss bedforms, as well as SE migration of NE-trending dune terminations. The SSE winds cause ephemeral dune deformation, especially crestal slipface reversals. Dune deformation occurs because of unequal deposition along the lee face as a function of the incidence angle formed between the wind and the local brinkline orientation. Incidence-angle control on dune deformation and types of lee-face surface processes allows for an idealized model for White Sands dunes. The dunes behave as complex systems in which each wind event deforms the dune shape, this new shape then serves as the configuration for the next wind event.<br>text
4
Ewing, Ryan Cotter. "Aeolian dune-field boundary conditions and dune interactions related to dune-field pattern formation on Earth and Mars." 2009. http://hdl.handle.net/2152/7561.
Full textAbstract:
Aeolian dune fields form some of the most striking patterns on Earth and Mars. These patterns reflect the internal dune dynamics of self-organization within boundary conditions, which are the unique set of environmental variables within which each dune field evolves. Dune-field pattern self-organization occurs because of interactions between the dunes themselves and the rich diversity of dune-field patterns arises because boundary conditions alter the type and frequency of dune interactions. These hypotheses are explored in three parts. First, source-area geometry and areal limits are two newly recognized boundary conditions. Measurements of crest length and spacing from satellite images of dune patterns with point and line source-area geometries show an increase in crest length and spacing over distance, whereas crest length and spacing in plane-sourced patterns emerge equally across the dune field. The areal limit boundary condition is the size and shape of the dune field itself. Empirical measurements from ten dune fields ranging over four orders of magnitude in area show that spacing increases and defect density decreases as the area of the dune field increases. A simple analytical model indicates that dune fields that are five times longer in the dune migration direction can achieve the greatest spacing for a given area. Second, time-series aerial photographs and airborne LiDAR show that fully developed, crescentic aeolian dunes at White Sands, New Mexico, interact and the dune pattern organizes in systematically similar ways as wind ripples and subaqueous dunes and ripples. Interaction type, classified as constructive, regenerative or neutral in terms of pattern development, changes spatially with the pattern because of the imposition of the line-source area and sediment availability boundary conditions. Upwind dominance by constructive interactions at the field line-source yields to neutral and regenerative interactions in the sediment availability-limited field center. Third, the dune-field pattern in the Olympia Undae Dune Field on Mars is comprised of two generations of dunes. This scenario of pattern reformation with a new wind regime shows that the emergence of the younger pattern is controlled by the boundary condition of the antecedent dune topography imposed upon the interaction between the younger and older patterns.<br>text
5
Eastwood, Erin Nancy. "Reconstructing environmental forcings on aeolian dune fields : results from modern, ancient, and numerically-simulated dunes." Thesis, 2011. http://hdl.handle.net/2152/25791.
Full textAbstract:
This dissertation combines studies of aeolian bedforms and aeolian dune-field patterns to create a comprehensive set of tools that can be used in tandem (or separately) to extract information about climate change and landscape evolution, and to identify the controls on formation for specific modern dune fields or ancient aeolian sequences. The spatial distribution of surface processes, erosion/deposition rates, and lee face sorting on aeolian dunes are each a function of the incident angle. This correlation between stratification style and incidence angle can be used to develop a “toolbox” of methods based on measurements of key suites of parameters found in ancient aeolian deposits. Information obtained from the rock record can be used as input data for different kinds of numerical models. Regional-scale paleowind conditions can be used to validate paleoclimate and global circulation models. Understanding the natural variability in the Earth’s climate throughout its history can help predict future climate change. Reconstructed wind regimes and bedform morphologies can be used in numerical models of aeolian dune-field pattern evolution to simulate patterns analogous to those reconstructed from ancient aeolian systems. Much of the diversity of aeolian dune-field patterns seen in the real world is a function of the sediment supply and transport capacity, which in turn determine the sediment availability of the system. Knowledge of the sediment supply, availability, and transport capacity of aeolian systems can be used to predict the amount of sand in the system and where it might have migrated. This information can be extremely useful for development and production of oil and gas accumulations, where a discovery has been made but the spatial extent of the aeolian reservoir is unknown.<br>text
Books on the topic "White Sands Dune Field"
1
Sale, Mark. A sea of sand: The White Sands Dune Field cultural resources survey, Holloman Air Force Base, Otero County, New Mexico. Geo-Marine, 1997.
Find full text
2
1950-, Collier Michael, ed. White Sands National Monument. Southwest Parks and Monuments Association, 1994.
Find full text
3
White Sands, official map and guide: White Sands National Monument, New Mexico. National Park Service, U.S. Dept. of the Interior, 1992.
Find full text
4
(Editor), Virgil W. Lueth, Katherine A. Giles (Editor), Spencer G. Lucas (Editor), Barry S. Kues (Editor), Robert Myers (Editor), and D. S. Ulmer-Scholle (Editor), eds. Geology of White Sands (Guidebook of the Field Conference). New Mexico Geological Society, 2002.
Find full textBook chapters on the topic "White Sands Dune Field"
1
Koster, Eduard. "Aeolian Environments." In The Physical Geography of Western Europe. Oxford University Press, 2005. http://dx.doi.org/10.1093/oso/9780199277759.003.0017.
Full textAbstract:
The literature on aeolian processes and on aeolian morphological and sedimentological features has shown a dramatic increase during the last decade. A variety of textbooks, extensive reviews, and special issues of journal volumes devoted to aeolian research have been published (Nordstrom et al. 1990; Pye and Tsoar 1990; Kozarski 1991; Pye 1993; Pye and Lancaster 1993; Cooke et al. 1993; Lancaster 1995; Tchakerian 1995; Livingstone and Warren 1996; Goudie et al. 1999). However, not surprisingly the majority of these studies discuss aeolian processes and phenomena in the extensive warm arid regions of the world. The results of aeolian research in the less extensive, but still impressive, cold arid environments of the world are only available in a diversity of articles. At best they are only briefly mentioned in textbooks on aeolian geomorphology (Koster 1988, 1995; McKenna-Neuman 1993). Likewise, the literature with respect to wind-driven deposits in western Europe is scattered and not easily accessible. The aeolian geological record for Europe, as reflected in the ‘European sand belt’ in the north-western and central European Lowlands, which extends from Britain to the Polish–Russian border, is known in great detail (Koster 1988; van Geel et al. 1989; Böse 1991). Zeeberg (1998) showed that extensive aeolian deposits progress with two separate arms into the Baltic Region, and into Belorussia and northernmost Ukraine. Recently, Mangerud et al. (1999) concluded that the sand belt extends even to the Pechora lowlands close to the north-western border of the Ural mountain range in Russia. Sand dunes and cover sands are widespread and well developed in this easternmost extension of the European sand belt. The northerly edges of this sand belt more or less coincide with the maximal position of the Late Weichselian (Devensian, Vistulian) ice sheet, while the southern edges grade into coverloams or sandy loess and loess (Mücher 1986; Siebertz 1988; Antoine et al. 1999). However, along these southern edges the dune fields and sand sheets regionally are derived from different sources, such as the sands of the Keuper Formation or the floodplains of the Rhine and Main rivers.
2
Westwood, Lisa, Beth Laura O’Leary, and Milford Wayne Donaldson. "Rocket Testing Sites." In The Final Mission. University Press of Florida, 2017. http://dx.doi.org/10.5744/florida/9780813062464.003.0004.
Full textAbstract:
“Rocket Testing Sites” presents some of the lesser known rocket testing sites founded with a better understanding of physics and rocketry provided by Goddard, beginning with the development of the V-2 and A-4 rockets. The chapter focuses on some histories of rocket testing involving Operation Paperclip and Werner Von Braun, such as the Saturn V and Redstone projects. It also focuses on memorable launching experimentation at a variety of facilities in the U.S., like the White Sands in New Mexico, the neighbouring Pioneer Deep Space Station, Cape Canaveral in Florida, the Edwards and Holloman Air Force Bases, and the Santa Susana Field Laboratory.
Conference papers on the topic "White Sands Dune Field"
1
Ewing, Ryan C., Gary Kocurek, David Mohrig, Virginia Smith, M. Hildegard Reiser, and David Bustos. "A DECADE OF THREE-DIMENSIONAL DUNE MORPHODYNAMIC OBSERVATIONS AT WHITE SANDS NATIONAL MONUMENT." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-282341.
Full text
2
Kramer, Henry D., Colton W. Byers, Gregory S. Baker, Paul Baldauf, and Patrick A. Burkhart. "DRONE ASSISTED INVESTIGATION OF DUNE FIELD MORPHOLOGY IN THE WHITE RIVER BADLANDS, SOUTH DAKOTA." In 54th Annual GSA Northeastern Section Meeting - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019ne-328224.
Full text
3
Kadir, Masran, Muhammad Ruzwin Rusli, Bukhari Samsudin, et al. "First Successful Installation of Through-Tubing Ceramic Sand Screen in Seligi Oil Field, Offshore Peninsular Malaysia." In International Petroleum Technology Conference. IPTC, 2021. http://dx.doi.org/10.2523/iptc-21440-ms.
Full textAbstract:
AbstractThe Seligi field, located 240 kilometers offshore peninsular Malaysia in the Malay basin was discovered in May 1971 and is one of the largest oil fields in Malaysia. Sand production in the Seligi field has been observed, especially from the J reservoirs group. Within the Seligi field, Well G was identified as one of the wells with sand production to surface that could lead to sand accumulation at surface facilities and erosion of equipment. Historically, there had been no in-situ sand control measures in the well. The default practice for sand control was to choke back the well, to prevent triggering of the surface sand probe (production with maximum sand-free rate). This approach however is a compromise, while it limits sand production, it also limits the production potential of the well (well technical potential). As part of the production enhancement assessment program, remedial sand-control methods were considered to increase the oil production while minimising sand production. Among the options considered was ceramic downhole sand screen installation. Ceramics have been used in many extreme erosion and corrosion applications, with ceramic sintered silicon carbide being 50 times harder than steel. Ceramic sand screens made with sintered silicon carbide offer much higher erosional resistance at speeds of 300ft/s sand impingement velocity. Due to the aggressive nature of the sands and high velocities of greater than 50ft/s in Well G, a through-tubing ceramic sand screen was selected. The ceramic sand screen served as a fit for purpose solution that allowed the well potential to be fully maximised, enabling a continuous production with minimal sand production at surface.This paper reviews the first successful pilot installation of through-tubing ceramic sand screen in Well G in the Seligi Oil Field, Offshore Peninsular Malaysia. Discussed are careful analysis and planning, i.e. velocity calculations, tool deployment simulations, tool inspections and detailed job procedure leading to a successful installation. With the ceramic sand screen installed, the well was able to produce at 100% production choke opening with lower tubing head pressure and has not produced sand at surface despite multiple shutdowns and well bean ups. The installation has also removed the need to have sand handling facilities at topside and has generated an implicated cost saving from expensive intervention programs. Given the success of this pilot installation, a baseline in sand control has been set for this field, with new well candidates being considered for future replication.
4
Shteynman, Leah, Brian Pinke, Edward C. V. Ruger, Katharine Wiley, Tamara L. Carley, and Ingrid Ukstins. "XRD ANALYSIS OF MAFIC SANDS FROM THE ICELANDIC INTERIOR: AN ANALOGUE STUDY FOR THE BAGNOLD DUNE FIELD OF MARS." In 54th Annual GSA Northeastern Section Meeting - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019ne-328469.
Full text
5
Abdul Wahab, Norsharmila, Muhammad Haniff Suhaimi, Aryanore Nafarine Antuni, et al. "Fluid Mapping-While-Drilling De-Risks Reservoir and Fluid Data Acquisition Workflow in a Brown Field." In IADC/SPE Asia Pacific Drilling Technology Conference. SPE, 2021. http://dx.doi.org/10.2118/201023-ms.
Full textAbstract:
Abstract Located offshore Malaysia, Field A is a highly complex elongated anticlinal structure with hundreds of faults. It includes over 70 hydrocarbon bearing sands deposited in a lower coastal plain environment. Producing since the late 1970s, Field A has gone through several asset rejuvenation plans. The latest one aimed at appraising and draining several untapped fault blocks. Although no major surprises were expected in terms of lithologies, uncertainties remained on fluids’ nature in multiple sands and on the possible isolation of the fault blocks. This paper illustrates how an operating company introduced a new while-drilling downhole formation fluid data acquisition workflow to successfully de-risk and address these challenges. Conventional formation evaluation is challenging in these fluvial environments, as it includes laminated reservoir, variable permeability, and presence of light, potentially saturated, hydrocarbons. Lessons learned from the previous rejuvenation campaign highlighted the importance of formation testing and downhole fluid analysis (DFA). The planned campaign required drilling two complex 3D profile wells (80-degree tangent followed by 35-degree drop through the targets). Pre-drill discussion raised various concerns: potential well control issues due to pumping light hydrocarbons in the borehole; sticking risk due to complex well trajectory and potential depletion; in-situ evaluation of CO2 for well deliverability analysis; and the number of logging runs, wiper, and post-drilling cleaning trips. In addition, the financial constraints on infill development called for the need of early, real-time enabled decisions for perforation and completion optimization. The selected drilling bottomhole assembly consisted of an integrated multi-physics logging-while-drilling toolstring including fluid mapping-while-drilling (FMWD) technology to de-risk the fluid acquisition program. The integration of pressures and DFA measurements with petrophysical data helped to identify and understand the distribution of fluids and fault blocks connectivity. The campaign proved to be very successful. All sand horizons were pressure tested, providing a fluid pressure profile description yielding gradients where applicable, differential pressure estimation, and connectivity information. The uncertainty associated with petrophysical fluid identification was addressed, and the use of FMWD showed no free gas in the tested zones. Fault block isolation was proven. Reservoir fluid and mobility profiling helped to optimize the well perforation and completion strategy and assess the producibility of the wells. The acquisition sequence was safely performed in one trip from bottom to top with no overpull observed. No wiper or post-drilling cleaning trips were required due to continuous mud circulation during data acquisition. This paper describes how this operating company successfully introduced a new while-drilling downhole formation fluid data acquisition workflow in a brown field. The workflow positively impacted the field development decisions. The FMWD de-risked data gathering operation under tight economical constraints and addressed formation evaluation and drilling and completion challenges during the evaluation of untapped blocks in Field A.
6
Zaitoun, Alain, Arnaud Templier, Jerome Bouillot, et al. "Successful Polymer Treatment of Offshore Oil Well Suffering from Sand Production Problems." In International Petroleum Technology Conference. IPTC, 2021. http://dx.doi.org/10.2523/iptc-21171-ms.
Full textAbstract:
Abstract Many fields in South East Asia are suffering from sand production problems due to sensitive sandstone formation. Sand production increases with time and increasing water production. The production of sand induces loss of production, due to sand accumulation in the wellbore, and heavy operational costs such as frequent sand cleaning jobs, pump replacements, replacement of surface and downhole equipment, etc. An original sand control technology consisting of polymers injection and already deployed in gas wells, has been successfully tested in an offshore oil well. The technology utilizes polymers having a natural tendency to coat the surface of the pores by a thin gel-like film of around 1 µm. Contrary to the use of resins which aim at creating a solid around the wellbore, the polymer system maintains the center of the pores fully open for fluid flow, thus preserving oil or gas permeability while often reducing water permeability (a property known as RPM for Relative Permeability Modification). The advantage of such system is that the product can be injected in the bullhead mode and often, a reduction of water production is observed along the drop in sand production. In gas wells, the treatment lasts around 4 years and can be renewed periodically. A lab work was undertaken to screen out a polymer product well suited to actual reservoir conditions. We conducted bulk tests to evaluate product interaction on reservoir sand samples, and corefloods to evaluate in-situ performances. Treatment volume and concentration were determined after lab test. One of "Oil Well" candidate is located in Arjuna Field, offshore Indonesia. Downhole conditions are: Temperature = 178°F, salinity = 18000 ppmTDS, permeability = 140-300mD, two perforated intervals with total thickness of 67ft (ft-MD) with 38 ft Average Netpay Thickness, production rate = 800 bfpd. The well is under gas lift and needed to be cleaned out every 3 months because of sand accumulation. Polymer treatment was performed in two stages (bottom, then upper interval). A total volume of 150 m3 of polymer solution was pumped. Immediately after treatment, sand cut dropped from 1% to almost 0%. This enabled increasing the drawdown from 32/64’’ choke to 40/64’’, keeping the production sand free and sustained with time. This field test confirms the feasibility of the original sand control polymer technology both in gas wells and in oil wells, which opens high possibilities in the future.
7
Kananithikorn, Nardthida, and Teenarat Songsaeng. "Pre-Drilled ECD Design by Using Fracture Pressure Model in Satun-Funan Fields, Pattani Basin, Gulf of Thailand." In International Petroleum Technology Conference. IPTC, 2021. http://dx.doi.org/10.2523/iptc-21368-ms.
Full textAbstract:
Abstract Lost circulation is the most common drilling issue for infill drilling projects in Satun-Funan Fields, South Pattani Basin, Gulf of Thailand (GOT). The depleted sand is possible to be a root cause in many wells based on observation from resistivity time-lapse separation in depleted sands or shale nearby. Therefore, the objective of this study is to estimate fracture pressure related to the depleted sand and design an appropriate Equivalent Circulating Density (ECD) threshold for each well to avoid or minimize lost circulation and well control complication during drilling a new well. This study model is using Eaton (1969) equation. There are 3 input parameters which are Poisson's Ratio and pre-drilled estimated depletion pressure and depth. With limitations of no actual fracturing data and limited sonic log, the maximum ECD while lost circulation reading from Pressure While Drilling (PWD) tool and formation pressure test data were used to back-calculate for Poisson's Ratio and identified a relationship with depth. From the total of 68 wells in the Satun and Funan areas, the interpreted Poisson's Ratio ranges from 0.36 to 0.44 and its linear trend is apparently increasing with depth. To minimize the variation of back calculated Poisson's Ratio the local data become an important key for model validation and maintain the similarity of subsurface factors. This interpreted Poisson's ratio trend will be used to calculate for fracture pressure by incorporating with estimated depletion pressure and depth that expect to encounter in each planned well. The lowest fracture pressure in a planned well is used to prepare pre-drilled ECD management plan and a real-time well monitoring plan. Additionally, the model can be adjusted during the operational phase based on the new drilled well result. This alternative model was applied in 4 trial drilling projects in 2019 and fully implement in 6 drilling projects in 2020. The lost circulation can be prevented with value creation from expected gain reserves section is $57M and cost avoidance from non-productive time due to lost circulation is $3.4M. With an effort, good communication and great collaboration among cross-functional teams, the model success rate increases by 12%. However, there are some unexpected lost events occurred even though the maximum ECD lower than expected fracture pressure. This suspect as a combination of limitations and uncertainties on key input parameters and drilling parameters. In the future, the model is planned to expand to other gas fields in the Pattani Basin which will move to more infill phase and have higher chance of getting lost circulation to maximize benefits as the success case in Satun and Funan fields.
8
El-Husseiny, Mahmoud, Taher El-Fakharany, and Samir Khaled. "The Innovative Integration of Wellbore Strengthening and Managed-Pressure Drilling Redraw the Line Between Undrillable and Drillable - Case Study from Offshore Mediterranean Deepwater." In SPE Annual Technical Conference and Exhibition. SPE, 2021. http://dx.doi.org/10.2118/206230-ms.
Full textAbstract:
Abstract Managed pressure drilling (MPD) has a reputation for enhancing drilling performance. However, in this study, we use it as a technology for making undrillable wells drillable. In the deepwater of the Mediterranean of Egypt, a gas field has been producing for few years. Water broke through in one well, thus, we must drill a new well to compensate for the reduction in production. Years of production led to pressure depletion, which makes it difficult to drill this well conventionally. In this study, we will discuss the combination of MPD and wellbore strengthening (WS). In addition, we will discuss the challenges we met while drilling and how we tackled them, and the best practices and recommendations for similar applications. The 12¼" × 13½" hole section passed depleted sands, followed by a pressure ramp. First, we drilled the depleted sands and confirmed the pressure ramp top. To strengthen the sand, we spotted a stress-cage pill of 645 bbls with a total concentration of 29 ppb. In addition, we conducted a formation integrity test (FIT), but its value was lower than the required value to drill to the section target depth (TD). Then, we switched to MPD and increased the mud weight. MPD in annular pressure control mode (AP) enabled us to walk the edge as near as possible to the impossible. Drilling this section was challenging due to the narrow mud weight window (MWW). We faced kick-loss cycles, where we had high-gas levels (from 20% to 55%) while drilling with a loss rate from 60 to 255 bph, at the same time. The 8½″ × 9½″ hole section will cover a depleted reservoir. Therefore, we decided to use the MPD to drill this section. To widen the MWW, we decided to stress-caging the hole, as we drill. We loaded the active-mud system with stress-cage materials totaling 39 ppb. We drilled the hole section while keeping the bottom hole pressure (BHP) at 14.6 ppg. We drilled using MPD by maintaining 525-psi surface back pressure (SBP). We used the SBP mode (semi-auto mode) to add connections, resulting in minor background gases and minor losses. This study discusses the application of a novel combination of MPD and WS. It emphasizes how MPD can integrate with other technologies to offer a practical solution to future drilling challenges in deepwater-drilling environments.
9
Al Enezi, D., M. AL Hajeri, S. Gholum, et al. "Realtime Drilling Geomechanics Aids Safe Drilling through Unstable Shales and Channel Sands of Wara Formations, Minagish Field, West Kuwait." In SPE Trinidad and Tobago Section Energy Resources Conference. SPE, 2021. http://dx.doi.org/10.2118/200929-ms.
Full textAbstract:
Abstract As part of any successful development plan of any hydrocarbon field, drilling boreholes safely is a key factor to make the entire process safe, economic and environmentally friendly. One of the main factors that dictates whether a borehole is going to be drilled safely or not is to understand the geomichanical behavior of the different formation to be penetrated. A definition of geomechanics could be stated as the science that studies the relationship between each of; in-situ stresses, rock mechanics, and the drilling fluid properties. In Kuwait and during the course of efforts to develop Wara channel sands in Minagish Field to the west of the country, Kuwait Oil Company (KOC) realized that continuing to drill development wells using conventional drilling practices is not any more an easy task. Considerable non-productive time has been recorded due encountering events such as shale carvings and pack off leading to stuck pipe. In addition, partial to total lost circulation were faced while drilling through Mutriba Formation which added to the complexity of problem. This study involved gathering data from offset wells to build a mechanical earth model for the area where the new well is going to be drilled. The main objective of having the model built is to perform wellbore stability analysis (WBS) and compute the quantitative mud window values to insure stable and safe borehole drilling. As the case of any study, performing reliable WBS analysis requires accurate modeling of earth stresses and rock mechanical properties. This process is primarily based on sonic logs (compressional and shear slowness), formation bulk density and lithology distribution. The study started with an audit of the available data sets in the region to select the best offset wells and generating empirical correlations to fill- up any missing and/or poor-quality data zones. Initially,7offset wells were identified, based on the geological distribution and data availability.Out of them, only four wells were found to have compressional slowness and three with bulk density measurements. However, it is worth mentioning that no shear slowness measurements were available in any of the offset wells in the region. Due to this, a correlation based compressional-shear relationship from nearby wells was proposed for the pre-drill study. The mechanical properties were characterized using the tri-axial core test results available from Wara and Burgan Formations. Empirical correlations were developed to obtain static mechanical properties from the dynamical mechanical ones and log responses. In addition, horizontal stresses in the region were constrained with formation integrity test data to have better control on the model. Finally, after the WBS model was built,it was compared to the available caliper data from the offset wells for calibration purposes. The resulted pre-drill geomechanics model was used to advise on the drilling parameters (mud weight) to be used in drilling the new development well. Moreover, and being the first realtime drilling geomechanics (RTDG) job in in Kuwait, an LWD sonic was used while drilling to supply the pre-drill model with realtime compressional and shear slowness measurements. Having the model updated in realtime with data from the formation at the borehole location resulted in optimizing the mud weight window limits by the geomechanics engineers as the well was being drilled. Following these mud weight recommendations based on the updated pre-drill model resulted in a smooth landing and horizontal sections in which all the wiper trips until the final pull out of hole were smooth.
10
Watcharasing, Sunisa, Surachai Lamsunthia, Yupin Phuphuak, Atipong Malatip, Yotsakorn Pratumwal, and Prapoj Kiattikomol. "Smart Facility Advanced Separator." In International Petroleum Technology Conference. IPTC, 2021. http://dx.doi.org/10.2523/iptc-21492-ms.
Full textAbstract:
Abstract The objective of this work was to develop the prototype unit of Advanced Production Separator (APS) for simultaneous removal of sand, out from production separator. APS unit was fabricated with size Diameter × Length: 1 × 2 m. System controlling of rotational blades impellers was installed at the bottom section of separator, to prevent sand accumulation at bottom of separator while on-service. This facility will help in preventing of sand accumulation in the separator, leading to minimize period of separator downtime during annual maintenance period, and allowing more working volume for open fluid reservoir to gas-oil phase production separator. Moreover, this will minimize working period for worker going inside the separator for sand clean-out, as a concern of working in the confine space. The optimum conditions for separation of sand and crude oil will be examined, with Computational Fluid Dynamics (CFD) model simulation to observe hydrodynamic flow, relating the experimental conditions. The effects of size of 1) Imperller shapes (model A, B, and C), and 2) Rotational speed of impellers (0, 50, 100, 150, and 200 rpm) were investigated to determine the optimal conditions for APS system. In this work, experimental test run result were compared with CFD simulation result. The optimum conditions for prototype APS unit (800 Litres capacity) is Fan C impeller shape for 5 items, and rotation speed for 150 rpm. This result shows the percentage of sand removal reaching to about 70%. The highest amount of sand in water outlet was found at this optimal condition, corresponding with the small part of sand dune at the bottom of the separator after impellers were driving sand to the outlet channel. From the test run, it was found that experimental results, and CFD simulation are consistent. CFD simulation result can be applied as a first screening to forecast sand removal pattern. This research illustrate the alternative novel solution for solving sand production accumulation problem in production separator, by instantly clear sand out while crude oil operation was on-going. In the future phase, CFD simulation will be further used as a first step for predicting result before separator scale-up. Separator will be experimented with 4-phases (oil, water, gas, and sand), and further expand for 4X of the original size to see an effect of scale-up. Aim to unlock high potential field, by reducing downtime of the separation during sand cleaning, and providing more working volume of separator after sand was removed out from self-cleaning separator.
Reports on the topic "White Sands Dune Field"
1
Quinn, Meghan. Geotechnical effects on fiber optic distributed acoustic sensing performance. Engineer Research and Development Center (U.S.), 2021. http://dx.doi.org/10.21079/11681/41325.
Full textAbstract:
Distributed Acoustic Sensing (DAS) is a fiber optic sensing system that is used for vibration monitoring. At a minimum, DAS is composed of a fiber optic cable and an optic analyzer called an interrogator. The oil and gas industry has used DAS for over a decade to monitor infrastructure such as pipelines for leaks, and in recent years changes in DAS performance over time have been observed for DAS arrays that are buried in the ground. This dissertation investigates the effect that soil type, soil temperature, soil moisture, time in-situ, and vehicle loading have on DAS performance for fiber optic cables buried in soil. This was accomplished through a field testing program involving two newly installed DAS arrays. For the first installation, a new portion of DAS array was added to an existing DAS array installed a decade prior. The new portion of the DAS array was installed in four different soil types: native fill, sand, gravel, and an excavatable flowable fill. Soil moisture and temperature sensors were buried adjacent to the fiber optic cable to monitor seasonal environmental changes over time. Periodic impact testing was performed at set locations along the DAS array for over one year. A second, temporary DAS array was installed to test the effect of vehicle loading on DAS performance. Signal to Noise Ratio (SNR) of the DAS response was used for all the tests to evaluate the system performance. The results of the impact testing program indicated that the portions of the array in gravel performed more consistently over time. Changes in soil moisture or soil temperature did not appear to affect DAS performance. The results also indicated that time DAS performance does change somewhat over time. Performance variance increased in new portions of array in all material types through time. The SNR in portions of the DAS array in native silty sand material dropped slightly, while the SNR in portions of the array in sand fill and flowable fill material decreased significantly over time. This significant change in performance occurred while testing halted from March 2020 to August 2020 due to the Covid-19 pandemic. These significant changes in performance were observed in the new portion of test bed, while the performance of the prior installation remained consistent. It may be that, after some time in-situ, SNR in a DAS array will reach a steady state. Though it is unfortunate that testing was on pause while changes in DAS performance developed, the observed changes emphasize the potential of DAS to be used for infrastructure change-detection monitoring. In the temporary test bed, increasing vehicle loads were observed to increase DAS performance, although there was considerable variability in the measured SNR. The significant variation in DAS response is likely due to various industrial activities on-site and some disturbance to the array while on-boarding and off-boarding vehicles. The results of this experiment indicated that the presence of load on less than 10% of an array channel length may improve DAS performance. Overall, this dissertation provides guidance that can help inform the civil engineering community with respect to installation design recommendations related to DAS used for infrastructure monitoring.