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Journal articles on the topic 'Kidson'

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Published: 26 July 2024

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1

Doolin, Ciaran. "Norway Comes to New Zealand: Edward Kidson, Jørgen Holmboe, and the Modernization of Australasian Meteorology." Bulletin of the American Meteorological Society 101, no. 12 (December 2020): E2095—E2112. http://dx.doi.org/10.1175/bams-d-20-0058.1.

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AbstractEdward Kidson, Director of the Meteorological Service of New Zealand from 1927 until his death in 1939, was an instrumental figure in modernizing Australasian meteorology. Throughout the 1920s, Kidson promoted the methods of synoptic analysis emanating from the Bergen School of Meteorology. However, it was not until the 1930s that he began in earnest to apply these methods to weather charts for the Australasian region. This development was aided by two visits he made to Bergen and by a personal correspondence he maintained with Jacob Bjerknes during the 1930s. In 1932, Kidson presented the first Norwegian-style analysis conducted for a Southern Hemisphere region, promptly following this with a more extensive study. However, these analyses were not of a sufficient standard at that stage to be adopted in forecasting practice. It was the fortuitous visit to New Zealand of Norwegian meteorologist Jørgen Holmboe, in 1934, that finally facilitated the transition. Holmboe was attached to the Lincoln Ellsworth Antarctic Expedition, but damage to their aircraft caused them to spend the winter of 1934 in New Zealand. Holmboe was engaged at the Meteorological Service in Wellington during this period, working with Kidson to apply Norwegian methods to the region. Kidson had hoped to further embed this practice by employing Tor Bergeron in New Zealand during 1938. Bergeron had accepted an offer from Kidson but canceled at the last minute after contracting rheumatic fever. Nevertheless, shortly after Holmboe’s visit, daily analyses were being conducted along Norwegian lines, bringing Australasian meteorology into the twentieth century.

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2

Robertson, Graham. "Kidson Island: a breeding site for Antarctic fulmars." Polar Record 27, no. 160 (January 1991): 61. http://dx.doi.org/10.1017/s0032247400019938.

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3

Francmanis, John. "The ‘Folk-Song’ Competition: An Aspect of the Search for an English National Music." Rural History 11, no. 2 (October 2000): 181–205. http://dx.doi.org/10.1017/s0956793300002090.

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On 10th April 1902 a sometime landscape artist and self-educated musical antiquarian took his seat in the Drill Hall at Kendal in Westmorland. Frank Kidson, an acknowledged authority on the subject, had been invited there to judge the first ever Folk-Song Competition. In introducing his guest the general adjudicator ‘could only say Mr Kidson was a walking encyclopoedia on these things’.The perceived need for a characteristically English art music bestowed considerable significance on folk-song, for both theory and practice in continental Europe suggested that such material comprised the essential ingredient of any such national music. To contextualise the importance of Kidson's task this article begins by briefly examining the condition of music in England in the late nineteenth century before considering the requirements to be made of this as yet largely untapped national resource.

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4

Zhan, Y. "A speculative ridge within the Kidson Sub-basin – integrated interpretation from geophysical data." Australian Energy Producers Journal 64, no. 1 (May 16, 2024): 242–57. http://dx.doi.org/10.1071/ep23112.

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This paper presents an analysis of the basement geometry and its implications on the Kidson Sub-basin in the southern Canning Basin. Integration of seismic data primarily near the rim of the sub-basin with airborne electromagnetic data across its central portion reveals an east-northeast oriented ridge at Permian level, suggesting a possible elevated structure in the Ordovician and basement. The proposed ridge effectively separates the Kidson Sub-basin into two distinct parts, providing an explanation for facies and thickness variations observed in the Nambeet and Goldwyer formations, as well as the absence of the Willara Formation in the southeastern portion of the sub-basin. The presence of shallowing trends observed in seismic profiles along the southern flank of the ridge suggests the proximity of the basement high. The ridge is speculative and requires further work to verify its existence, potentially including passive and reflection seismic surveys across the structure. If confirmed, it might be a significant feature with far-reaching implications for the prospectivity of resources in the Kidson Sub-basin. The hydrocarbon sourced from the Nambeet, Goldwyer and Bongabinni formations in the NNW depocentre may have migrated via the extension of the Parallel Range Fault and be trapped in the footwall block over the ridge. Compared to the structures in the Fitzroy Trough, the traps within the Kidson Sub-basin are expected to maintain reasonable integrity and have good potential for petroleum accumulation and carbon sequestration in the thick Paleozoic succession.

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5

Crossley, Paul, and Peter Draper. "Professor Peter Kidson: 23 August 1925 – 10 February 2019." Journal of the British Archaeological Association 172, no. 1 (January 1, 2019): 176–78. http://dx.doi.org/10.1080/00681288.2019.1642011.

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6

Southby, Chris, Lidena Carr, Paul Henson, Peter Haines, Alex Zhan, Jade Anderson, Susannah MacFarlane, Tanya Fomin, and Ross Costelloe. "Exploring for the future: Kidson Sub-basin seismic interpretation." ASEG Extended Abstracts 2019, no. 1 (November 11, 2019): 1–3. http://dx.doi.org/10.1080/22020586.2019.12073007.

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7

Barlow, Mike. "Geoscience Australia: GADDS release, Kidson Sub-basin 2D seismic survey and new AusLAMP results." Preview 2020, no. 208 (September 2, 2020): 17–19. http://dx.doi.org/10.1080/14432471.2020.1828393.

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8

Francmanis, John. "National music to national redeemer: the consolidation of a ‘folk-song’ construct in Edwardian England." Popular Music 21, no. 1 (January 2002): 1–25. http://dx.doi.org/10.1017/s0261143002002015.

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The Musical Renaissance of the late Victorian era incurred both rediscovery and reappraisal of the English musical heritage. The isolated endeavours of a handful of pioneering collectors from the oral tradition stimulated the institution of a Folk-Song Society with the aim of gathering what remained of a rapidly disappearing national resource. This article examines competing interpretations of the nature and potential application of folk-song. Cecil Sharp, who quickly assumed leadership of the folk-song movement, adopted and refined the notion that communal origin and transmission imbued folk-song with the national character and spirit. Its strategic use in the education system would, he believed, promote not just musical revival but a general national revival as well. In counterpoint to Sharp's folk-song construct, the hiterto marginalised contribution of musical antiquarian Frank Kidson is reassessed. From an ever-diminishing position of authority, Kidson continued to dismiss Sharp's new orthodoxy by insisting that most of what passed for ‘folk’ was nothing more than the remnants of old popular song. The article concludes by seeking to explain why Sharp's construct endured.

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9

Rohr, David M. "Color banding in Texigryphaea (Bivalvia) from the Cretaceous of west Texas." Journal of Paleontology 62, no. 01 (January 1988): 147–48. http://dx.doi.org/10.1017/s0022336000059023.

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A single specimen of Texigryphaea navia (Hall) was recovered from Albian (Lower Cretaceous) rocks 35 km (22 mi) east of Ft. Stockton, Texas, along the north side of Interstate Highway 10 (104°52′N, 102°32′W) opposite a rest area. The fossil is from a semiconsolidated marl unit mapped on the Ft. Stockton 1:250,000 Geologic Atlas of Texas (Barnes, 1982) as Washita Group and referred to as the Ft. Lancaster Formation by Scott and Kidson (1977).

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10

Barnes,, Carl F. "Review: Medieval Architecture and Its Intellectual Context: Studies in Honour of Peter Kidson by Eric Fernie, Paul Crossley." Journal of the Society of Architectural Historians 51, no. 1 (March 1, 1992): 92–93. http://dx.doi.org/10.2307/990646.

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11

Fauchereau, N., B. Pohl, and A. Lorrey. "Extratropical Impacts of the Madden–Julian Oscillation over New Zealand from a Weather Regime Perspective." Journal of Climate 29, no. 6 (March 15, 2016): 2161–75. http://dx.doi.org/10.1175/jcli-d-15-0152.1.

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Abstract The Madden–Julian oscillation (MJO) signal in the Southern Hemisphere (SH) extratropics during the austral summer (November–March) is investigated over the New Zealand (NZ) sector, using the paradigm of atmospheric weather regimes (WRs), following a classification initially established by Kidson. The MJO is first demonstrated to have significant impacts on daily rainfall anomalies in NZ. It is suggested that orographic effects arising from the interaction between regional atmospheric circulation anomalies and NZ’s topography can explain the spatially heterogeneous precipitation anomalies that are related to MJO activity. These local impacts and circulation anomalies are shown to be better understood as resulting from changes in the occupation statistics of regional WRs (the Kidson types) through the MJO life cycle, although both constructive and destructive effects are demonstrated. The hypothesis of a significant forcing of the MJO over the NZ sector is further supported by lagged composite analyses, which reveal timing characteristics of the delayed regional circulation response compatible with the average propagation speed of the MJO. While the southern annular mode (SAM) has been previously shown to be statistically related to the MJO and is known to be a significant driver of NZ’s climate, no evidence is found that the impact of the MJO over the NZ sector is mediated by the SAM. It is therefore suggested that the MJO directly impacts regional circulation and climate in the NZ region, potentially through extratropical Rossby wave response to tropical diabatic heating. These findings suggest a new potential for predictability for some aspects of NZ’s weather and climate deriving from the MJO beyond the meteorological time scales.

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12

Dandrea, Ruth Ann. "Kidsong." English Journal 93, no. 2 (November 2003): 58. http://dx.doi.org/10.2307/3650497.

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13

Dandrea, Ruth Ann. "Kidsong." English Journal 93, no. 2 (November 1, 2003): 58–60. http://dx.doi.org/10.58680/ej20032637.

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14

Bailey, Adam H. E., Amber J. M. Jarrett, Liuqi Wang, David N. Dewhurst, Lionel Esteban, Shane Kager, Ludwig Monmusson, Lidena K. Carr, and Paul A. Henson. "Exploring for the Future geomechanics: breaking down barriers to exploration." APPEA Journal 61, no. 2 (2021): 579. http://dx.doi.org/10.1071/aj20039.

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Exploring for the Future (EFTF) is an Australian Government initiative focused on gathering new data and information about potential mineral, energy and groundwater resources across Australia. The energy component of EFTF, initially focussed on northern Australia, aims to improve our understanding of the petroleum potential of frontier Australian basins. Building an understanding of geomechanical rock properties is key to understanding both conventional and unconventional petroleum systems as well as carbon storage and sedimentary geothermal systems. Under EFTF, Geoscience Australia has undertaken geomechanical work including stress modelling, shale brittleness studies and the acquisition of new rock property data through extensive testing on samples from the Paleo- to Mesoproterozoic South Nicholson region of Queensland and the Northern Territory, and the Paleozoic Kidson Sub-basin of Western Australia. Work in these regions demonstrates regional stress orientations in broad agreement with previously modelled, continent-scale stress orientations and stress magnitudes that vary through the basin with depth and by lithology. Rock testing highlights potentially brittle shales and demonstrates variable rock properties in line with lithology. These analyses are summarised herein. Providing baseline geomechanical data in frontier basins is essential as legacy data coverage can often be inadequate for making investment decisions, particularly where unconventional plays are a primary exploration target. As EFTF increases in scope, Geoscience Australia anticipates expanding these studies to encompass further underexplored regions throughout Australia, lowering the barrier to entry and encouraging greenfield exploration.

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15

Ghori, Ameed. "New heat flow data aids exploration in the Canning Basin, Western Australia." APPEA Journal 50, no. 1 (2010): 411. http://dx.doi.org/10.1071/aj09025.

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The Geological Survey of Western Australia (GSWA) is providing new heat flow data and continuing studies in subsurface temperatures to understand the origin, migration and accumulation of geofluids in petroleum and geothermal systems of the Canning Basin. The study includes an investigation of subsurface temperatures from 274 wells, thermal conductivity measurement of 50 core samples from 22 wells, and single-dimensional (1D) heat-flow modelling of 101 wells. Thermal conductivity measurement of Canning Basin formations range from 1.06–5.83 W/mºC and modelled surface heat-flow ranges from 20–160 mW/m². The lowest measured thermal conductivity is in the Ordovician Goldwyer Formation at 1.06± 0.28 W/mºC, and the highest values are in the Upper Carboniferous Reeves Formation at 5.83 ± 0.22 W/mºC. Generally, estimated heat-flow values are lower where thick sedimentary deposits are present such as the Fitzroy Trough, Lennard Shelf, and Kidson Sub-basin, with values less than 65 mW/m². The heat flow values increase to over 80 mW/m² on the Broome Platform and Jurgurra, Mowla and Barbwire terraces. Lower heat-flow values have been modelled in West Blackstone–1 (47 mW/m²), Curringa–1 (52 mW/m²), Kennedia–1, Napier–2 and Pearl–1 (55–52 mW/m²). Higher heat-flow values have been modelled in Goodenia–1, Lovells Pocket–1, Kanak–1, Cudalgarra North–1, and Cudalgarra–1, where heat-flow values are over 100 mW/m². These new thermal conductivities, corrected temperatures, and heat-flow values support improved modelling of the Canning Basin petroleum and geothermal systems.

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16

Haines, Peter. "The Carribuddy Group and Worral Formation, Canning Basin, Western Australia: reassessment of stratigraphy and petroleum potential." APPEA Journal 50, no. 1 (2010): 425. http://dx.doi.org/10.1071/aj09026.

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Reassessment of stratigraphic relationships and biostratigraphic data pertaining to the Carribuddy Group and Worral Formation in all relevant petroleum wells and many mineral drill holes across the southern Canning Basin has led to the following important results. The Carribuddy Group is restricted to the Late Ordovician to earliest Silurian. The overlying Worral Formation is mostly of Silurian age and does not intertongue with the Middle Devonian Tandalgoo Formation, as previously thought. A thin basin-wide chronostratigraphic marker—the Pegasus Dolomite Member (previously referred to as dolomite spike or dolomite marker) of the Sahara Formation—allows improved correlation between salt-bearing sub-basins and adjacent condensed Carribuddy Group successions. The Mallowa Salt is not as extensive as previously thought; rather the Minjoo Salt thickens to become the only salt seal in the eastern and southern Kidson Sub-basin. The Carribuddy Group forms the regional seal to the prospective Larapintine 2 petroleum system, but also contains local source and reservoir facies. The Bongabinni Formation contains extremely rich oil-prone source rocks in local lagoonal facies along the Admiral Bay Fault Zone; these rocks have been linked by other studies to migrated oil in that area. The distribution of the source facies is poorly known, but it may extend down-dip into more mature parts of the Willara Sub-basin, and west into offshore areas. Other local source units may be present in the Mallowa Salt, and possibly the Nibil Formation, but are not well documented. Aeolian sandstone with excellent reservoir potential is locally present in the Nibil Formation, but is more extensive in the lower Worral Formation, particularly the Elsa Sandstone Member.

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17

Knight, D. A., and V. G. Medina. "Kidston gold mines startup." Mining, Metallurgy & Exploration 3, no. 1 (February 1986): 45–49. http://dx.doi.org/10.1007/bf03402635.

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18

Smith, David Canfield, Allen Cypher, and Jim Spohrer. "KidSim." Communications of the ACM 37, no. 7 (July 1994): 54–67. http://dx.doi.org/10.1145/176789.176795.

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19

Zhan, Y. "Velocity anomalies and out-of-plane reflections in Barnicarndy 1, Canning Basin." APPEA Journal 61, no. 1 (2021): 271. http://dx.doi.org/10.1071/aj20082.

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Barnicarndy 1 was drilled as a stratigraphic well and penetrated 2585m of clastic sedimentary rocks overlying an angular unconformity composed of Proterozoic dolomite basement near SSE end of the eponymous graben (previously known as the Waukarlycarly Embayment) of the Canning Basin. The post-drilling data exhibited several types of anomalies and inconsistencies, including ultra-slow velocity of the vertical seismic profile (VSP) within the top 210m, substantially high velocity from 210 to 1390m, poor synthetic–seismic correlation, and discrepancies between the prognosis and actual depths. The VSP shows that the uppermost sedimentary section has an average velocity of less than 1000m/s, which is unrealistically slow and probably caused by a systematic time delay in the data acquisition. Such a delaying effect was removed when calculating the VSP interval velocity, which had reasonable consistencies with sonic velocity and lithological packages. The consistencies verify that the sections from 210 to 1390m have high velocities that are beyond the range of offset wells at equivalent depths and do not follow an expected trend along most of the well trajectory. Quantitative analyses of multiple synthetic correlations suggest that the depth discrepancies in the prognosis are not related to pre-drilling seismic interpretation, as the two-way time picks for major boundaries mostly match what has been penetrated in Barnicarndy 1. Two thirds of the depth error for basement prognosis comes from the unexpected high velocity in the shallow formations. The velocity anomalies indicate that the Barnicarndy Graben possibly has a complex history of tectonic movement, and thick sections could have been eroded during the Late Triassic. The remaining discrepancy in depth prognosis for the basement is related to the out-of-plane seismic reflection near the SSE end of the graben. The steeply dipping basement causes out-of-plane issues for 2D seismic data, and the Kidson seismic survey images the shallower basement reflected from further south, rather than what is vertically below the survey route.

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20

Normore, Leon, Peter W. Haines, Lidena K. Carr, Paul Henson, Yijie Zhan, Michael T. D. Wingate, Yong Yi Zhen, et al. "Barnicarndy Graben, southern Canning Basin: stratigraphy defined by the Barnicarndy 1 stratigraphic well." APPEA Journal 61, no. 1 (2021): 224. http://dx.doi.org/10.1071/aj20160.

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Funded by Geoscience Australia’s Exploring for the Future initiative and operated by the Geological Survey of Western Australia, the Waukarlycarly 1 deep stratigraphic drillhole was designed to investigate the geology of the little-known Waukarlycarly Embayment and assess the petroleum, mineral, groundwater and CO2 storage potential of the area. Based on consultation with the Western Desert Lands Aboriginal Corporation on the cultural significance of the name, Waukarlycarly, it has been agreed to change the name of the well to Barnicarndy 1 and the tectonic subdivision to the Barnicarndy Graben. This and all future publications will now refer to the Barnicarndy 1 stratigraphic drillhole (previously Waukarlycarly 1) and the Barnicarndy Graben (previously Waukarlycarly Embayment). Drilling commenced on 1 September 2019 and reached a total depth (TD) of 2680.53m on 30 November 2019, recovering more than 2km of continuous core. The cored interval extended from 580m to TD in Neoproterozoic Yeneena Basin dolostone, which was unconformably overlain by a thick, lower Canning Basin Ordovician stratigraphy, including richly fossiliferous marine mudstones with common volcanic ash beds. A major unconformity is located at the top of the Ordovician section where it is overlain by sandstones and muddy diamictites of the Carboniferous–Permian Grant Group, followed by a Cenozoic succession near surface. Ditch cuttings were collected from surface to 580m at 3m intervals. The pre-Grant Group Paleozoic succession is unique within the Canning Basin, indicating that the Barnicarndy Graben’s depositional history is markedly different when compared with adjacent structural subdivisions, such as the Munro Arch and Kidson Sub-basin. Detrital zircon geochronology, biostratigraphy and borehole imaging interpretation assisted in the definition of two new geological units within the Ordovician stratigraphy of Barnicarndy 1: the Yapukarninjarra and Barnicarndy formations. Preliminary routine core analysis data indicates the potential for CO2 storage within the Barnicarndy Formation beneath a Grant Group seal. The well also provides new insights into the structural interpretation of the Barnicarndy Graben.

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21

Kapeliuk, Amnon. "Kidron: Refusenik!! Israel's Soldiers of Conscience." Journal of Palestine Studies 34, no. 1 (2004): 92–93. http://dx.doi.org/10.1525/jps.2004.34.1.92.

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22

Bartrum, J., A. Bowler, and G. Butcher. "SAG mill operations at Kidston Gold Mines." Mining, Metallurgy & Exploration 3, no. 2 (May 1986): 96–104. http://dx.doi.org/10.1007/bf03402645.

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23

Alexandra A. Taylor. "SLCC chem club holds KidCon outreach event." C&EN Global Enterprise 99, no. 40 (November 1, 2021): 35. http://dx.doi.org/10.1021/cen-09940-acsnews1.

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24

Warris, B. J. "THE HYDROCARBON POTENTIAL OF THE PALAEOZOIC BASINS OF WESTERN AUSTRALIA." APPEA Journal 33, no. 1 (1993): 123. http://dx.doi.org/10.1071/aj92010.

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There are four main Palaeozoic Basins in Western Australia; the Perth Basin (Permian only), the Carnarvon Basin (Ordovician-Permian), the Canning Basin (Ordovician-Permian) and the Bonaparte Basin (Cambrian-Permian).The Perth Basin is a proven petroleum province with commercially producing gas reserves from Permian strata in the Dongara, Woodada and Beharra Springs gas fields.The Palaeozoic of the Carnarvon Basin occurs in three main sub-basins, the Ashburton, Merlinleigh and Gascoyne Sub-basins. No commercial petroleum discoveries ahve been made in these basins.The Canning Basin can be divided into the southern Ordovician-Devonian province of the Willara and Kidson sub-basins and Wallal Embayment and Anketell Shelf, and the northern Devonian-Permian province of the Fitzroy and Gregory sub-basins. Commercial production from the Permo-Carboniferous Sundown, Lloyd, West Terrace, Boundary oilfields and from the Devonian Blina oilfield is present only in the Fitzroy sub-basins.The Bonaparte Basin contains Palaeozoic strata of Cambrian-Permian age but only the Devonian-Permian is considered prospective. Significant but currently non-producing gas discoveries have been made in the Permian of the Petrel and Tern offshore gas fields.Based on the current limited well control, the Palaeozoic basins of Western Australia contain excellent marine and non marine clastic reservoirs together with potential Upper Devonian and Lower Carboniferous reefs. The dominantly marine nature of the Palaeozoic provides thick marine shale seals for these reservoirs. Source rock data is very sparse but indicates excellent gas prone source rocks in the Early Permian and excellent—good oil prone source rocks in the Early Ordovician, Late Devonian, Early Carboniferous and Late Permian.Many large structures are present in these Palaeozoic basins. However, most of the existing wells were drilled either off structure due to insufficient and poor quality seismic or on structures formed during the Mesozoic which postdated primary hydrocarbon migration from the Palaeozoic source rocks.With modern seismic acquisition and processing techniques together with a better understanding of the stratigraphy, structural development and hydrocarbon migration, the Palaeozoic basins of Western Australia provide the explorer with a variety of high risk, high potential plays without the intense bidding competition currently present along the North West Shelf of Australia.

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25

Edwards, C. J. W., D. McCourt, P. J. Duffy, F. H. A. Aalen, A. A. Horner, Robert D. Osborne, Colin A. Lewis, et al. "Reviews of Books and Maps." Irish Geography 11, no. 1 (December 26, 2016): 199–213. http://dx.doi.org/10.55650/igj.1978.845.

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AGRICULTURE IN THE REPUBLIC OF IRELAND, by Desmond A. Gillmor (Geography of world agriculture, volume 7). Budapest: Akademiai Kiado, 1977. 202 pp.PEASANT OPENFIELD FARMING AND ITS TERRITORIAL ORGANISATION IN COUNTY TIPPERARY, by Ingeborg Leister.Marburg: Marburger Geographische Schriften, 1976. 100 pp.SOURCES FOR LOCAL STUDIES, by William Nolan. Department of Geography, Carysfort College, 1977, 61 pp.COUNTY LEITRIM RESOURCE SURVEY. Part III ‐ Demography, Sociology and Economics. Dublin: An Foras Taluntais, 1975. 101 pp. £2.00.THE DEVELOPMENT OF THE IRISH TOWN, edited by R. A. Butlin. London: Croom Helm, 1977. 144 pp. £6.95.NATIONALISM AND SOCIALISM IN TWENTIETH‐CENTURY IRELAND, by E. Rumpf and A. C. Hepburn. Liverpool: the University Press, 1977. 275 pp. £15–25.THE QUATERNARY HISTORY OF THE IRISH SEA, edited by C. Kidson and M. J. Tooley. Liverpool: Seel House Press, 1977. 345 pp. £16.00.MEDIEVAL MOATED SITES OF S.E. IRELAND, by Terence B. Barry. London: British Archaeological Reports, 35, 1977. 247 pp., £4.70.LIFE AND TRADITION IN RURAL IRELAND, by Timothy P. O'Neill. London: J. M. Dent & Sons, 1977. 122 pp. £9.95.SERVICE‐TYPE EMPLOYMENT AND REGIONAL DEVELOPMENT, by Michael J. Bannon, James G. Eustace and Mary Power. Dublin: Stationery Office, National Economic and Social Council report no. 28, undated (1977) 142 pp. £0.55.CONSUMER BEHAVIOUR, MOTIVATION AND PERCEPTION : A STUDY OF DUBLIN, by A. J. Parker. Dublin: Department of Geography, University College, 1976. 265 pp. £2.50.SOILS OF COUNTY WESTMEATH, by T. F. Finch. Dublin: An Foras Taluntais, National Soil Survey of Ireland, Soil Survey Bulletin No. 33, 1977. 100 pp. £5.THE SUGAR INDUSTRY IN IRELAND, by Michael Foy. Dublin: Comhlucht Siúicre Éireann Teo., 1976. 159 pp.THE RELEVANCE OF THE INTERNATIONAL HYDROLOGICAL DECADE TO ULSTER, by R. Common. Belfast: Department of Geography, Queen's University, Departmental Research Paper No. 1, 1977. 160 pp.THE CHANGING FORTUNES OF MARGINAL REGIONS, edited by P. G. Sadler and G. A. Mackay. Aberdeen: Institute for the Study of Sparsely Populated Areas, undated. 163 pp. £2.85.DUBLIN'S WOOD QUAY, by Nuala Burke. Drumconrath: Civic Heritage Publications, 1977. 46 pp. £3.30.MAP REVIEWTHE BURREN: A MAP OF THE UPLANDS OF NORTH‐WEST CLARE, EIRE, by T. D. Robinson: Cill Ronain, published by the author, 1977. 92 cm × 65 cm. £1.10.

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26

Showstack, Randy. "KidSat Kodak moments." Eos, Transactions American Geophysical Union 78, no. 45 (1997): 506. http://dx.doi.org/10.1029/eo078i045p00506-02.

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27

Way, J., J. D. Baker, P. Andres, J. McGuire, M. Galindo, J. Fox, and E. J. Stork. "The KidSat project." IEEE Transactions on Geoscience and Remote Sensing 37, no. 4 (July 1999): 1753–67. http://dx.doi.org/10.1109/36.774689.

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28

Albandary Alamer, Noura Alaskar, Sana Bukhamseen, Jawaher Alkhamis, Enas Alghamdi, and Almaha Almulhim. "Design and prototyping of Kiddo, a mobile application for parents to control kids' learning." Global Journal of Information Technology: Emerging Technologies 12, no. 1 (April 30, 2022): 59–68. http://dx.doi.org/10.18844/gjit.v12i1.7432.

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A good and healthy seed will always produce a nice fruit, whereas an infected seed will produce an infected fruit. The same concept applies to children; the healthier the environment in which the kids grow, the more likely they become valuable members of society. Therefore, this study aimed to design an app that aims to enhance the communication between parents and their children and enrich the good habits of the kid. This paper will mainly discuss the proposed idea and its design, as also it is mentioning the app’s main functionalities. The Kiddo project introduces us to a mobile application that focuses on enhancing the sense of responsibility from a young age and makes raising kids fun and easy. Kiddo Application enables kids to share their accomplishments with their peers in an interactive environment full of enjoyment followed by parental monitoring to handle what their kids are posting and friends following. Keywords: Educational app; Kiddo; Kids; parental control; social media.

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29

Thomson, Christine A., and Ian P. Wilkinson. "Robert Kidston (1852–1924): biography of a Scottish palaeobotanist." Scottish Journal of Geology 45, no. 2 (October 1, 2009): 161–68. http://dx.doi.org/10.1144/0036-9276/01-360.

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SynopsisThis brief biography summarizes the life of Scots-born Robert Kidston (1852–1924), who was arguably the best and most influential palaeobotanist of his day. In over 180 scientific papers he laid the foundations for a modern understanding of the taxonomy and palaeobiology of Devonian and Carboniferous plants. His expertise was critical to the research and curation of the Geological Survey and British Museum (Natural History) and excavations of Glasgow's Fossil Grove introduced the great Carboniferous forests into the public imagination. Despite their age, his meticulously documented collections of slides (deposited in the Botany collection University of Glasgow) and hand specimens and notebooks (deposited in the collections of the British Geological Survey, Nottingham) provide a wealth of important scientific data with modern applications in plant taxonomy, biostratigraphy and palaeoclimatic reconstruction.

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Bensignor, François. "Angélique Kidjo." Hommes & migrations, no. 1331 (November 17, 2020): 235–41. http://dx.doi.org/10.4000/hommesmigrations.12061.

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Pini, Barbara, and Martin Mills. "Constructing the rural in education: the case ofOutback Kidsin Australia." British Journal of Sociology of Education 36, no. 4 (November 29, 2013): 577–94. http://dx.doi.org/10.1080/01425692.2013.829745.

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Grohs, K., and A. Marton. "The Evolution of Wall Control Programs at Kidston Gold Mines." Fragblast 6, no. 3-4 (December 1, 2002): 345–58. http://dx.doi.org/10.1076/frag.6.3.345.14050.

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Baker, J. D., J. Woodring, A. Leach, J. Lane, and R. Spohr. "The KidSat project flight system." IEEE Transactions on Geoscience and Remote Sensing 37, no. 4 (July 1999): 1768–74. http://dx.doi.org/10.1109/36.774690.

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34

Tseng, C., N. Hung, and S. Jue. "KidSat views 1997 Indonesia fires." IEEE Transactions on Geoscience and Remote Sensing 37, no. 4 (July 1999): 1827–33. http://dx.doi.org/10.1109/36.774695.

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Acharya, Anurag, Sudipta Bhawmik, C. R. K. Prasad, and P. Palchaudhuri. "KIDLAN: A hardware description language." Microprocessing and Microprogramming 26, no. 1 (March 1989): 1–13. http://dx.doi.org/10.1016/0165-6074(89)90276-7.

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36

Alfano, Andrea. "Kiddo Knows Best." Scientific American 312, no. 6 (May 19, 2015): 25. http://dx.doi.org/10.1038/scientificamerican0615-25.

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Hass, Hagen. "The epidermis of Hornephyton lignieri (KIDSTON & LANG) BARGHOORN & DARRAH." Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen 183, no. 1-3 (December 20, 1991): 61–85. http://dx.doi.org/10.1127/njgpa/183/1991/61.

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Gersberg, Betina. "Kidbox, un mundo feliz en Internet." Dixit, no. 16 (September 9, 2012): 44–48. http://dx.doi.org/10.22235/d.v0i16.346.

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En un almuerzo familiar de sábado, Alan Kind, ingeniero en computación interesado en aplicaciones web, y Martin Larre, abogado con experiencia en la venta de productos editoriales infantiles, conversaban sobre la problemática aún no resuelta en torno al vínculo de los niños e Internet. Notaron que los padres querían usar la red de la mejor manera, pero que esa intención era relegada por el miedo que le tenían. Entonces, con esos dos pilares como objetivos, la de maximizar la experiencia del medio y la de experimentarlo con seguridad, surgió la idea de crear una solución que diera respuesta a esas dos necesidades. Es así que, además de cuñados, estos profesionales se convirtieron en socios fundadores de Kidbox.

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39

Jones, Mark, and Lesley Mackay. "KidSat: Students Exploring Earth from Space." Imagine 4, no. 3 (1997): 6–7. http://dx.doi.org/10.1353/imag.2003.0053.

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Yedes, Janet. "Playful Teasing: Kiddin' on the Square." Discourse & Society 7, no. 3 (July 1996): 417–38. http://dx.doi.org/10.1177/0957926596007003006.

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Christoffel, K. K., and J. L. Schofer. "Evaluation of a systematic approach for identifying injury scenarios. Kids'n' Cars Teams." Injury Prevention 2, no. 3 (September 1, 1996): 221–27. http://dx.doi.org/10.1136/ip.2.3.221.

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Barak, Boaz. "Environmental Economic Approach for Resolving the Environmental Crisis in Jerusalem’s Kidron River Basin." International Journal of Science in Society 3, no. 2 (2012): 65–78. http://dx.doi.org/10.18848/1836-6236/cgp/v03i02/51326.

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Sansom, Clare. "Rosalind Franklin, Nicole Kidman and Photograph 51." Biochemist 37, no. 6 (December 1, 2015): 45–46. http://dx.doi.org/10.1042/bio03706045.

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Swiger, Molly. "Nicole Kidman. PamCook. London: Palgrave Macmillan, 2012." Journal of American Culture 36, no. 2 (June 2013): 147–48. http://dx.doi.org/10.1111/jacc.12020_13.

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Abend-David, Dror. "Shakespeare, Nicole Kidman and Contemporary Translation Theory." FORUM / Revue internationale d’interprétation et de traduction / International Journal of Interpretation and Translation 10, no. 2 (October 1, 2012): 1–18. http://dx.doi.org/10.1075/forum.10.2.01abe.

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Rackley, K. "The KidSat Student Mission Operations Center-SMOC." IEEE Transactions on Geoscience and Remote Sensing 37, no. 4 (July 1999): 1775–84. http://dx.doi.org/10.1109/36.774691.

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MARUYAMA, Toshiaki. "ARCHITECTURAL STYLE OF KIDOMON IN KYOTO : A study on Kidomon of Kyoto in the Edo era (No.2)." Journal of Architecture and Planning (Transactions of AIJ) 69, no. 575 (2004): 139–45. http://dx.doi.org/10.3130/aija.69.139_1.

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Bui, X. N., T. H. Nguyen, V. L. Nguyen, K. Kikuchi, T. Nagai, T. M. Nguyen, T. N. Nguyen, et al. "144 EFFECTS OF CO-CULTURE WITH FIBROBLASTS AND OVIDUCT CELLS ON IN VITRO PRODUCTION OF PORCINE EMBRYOS." Reproduction, Fertility and Development 25, no. 1 (2013): 219. http://dx.doi.org/10.1071/rdv25n1ab144.

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Cell co-culture during in vitro maturation or embryo culture has been reported as a method to improve the efficiency of maturation or embryo development (Kidson et al. 2003 Theriogenology 59, 1889; Romar et al. 2005 Anim. Reprod. Sci. 85, 287). Here, we present the impact of different methods of co-culture with mouse embryonic fibroblasts or oviduct epithelial cells on in vitro embryo production in pigs. Cumulus–oocyte complexes (COC) were collected from follicles with diameter larger than 3 mm and used for in vitro embryo production based on the method of Kikuchi et al. 2002 (Biol. Reprod. 66, 1033) with minor modifications. There were 8 groups; group 1: maturation and embryo culture without cell co-culture (control group); group 2: maturation in the presence of fibroblasts; group 3: embryo culture in the presence of fibroblasts; group 4: both maturation and embryo culture in the presence of fibroblasts; group 5: maturation in the presence of oviduct cells; group 6: embryo culture in the presence of oviduct cells; group 7: both maturation and embryo culture in the presence of oviduct cells; group 8: both maturation and embryo culture in the presence of both fibroblast and oviduct cells. In vitro maturation (IVM) was carried out at 39oC under 5% CO2 in air for 44 h using NCSU-37 as basic medium. Matured oocytes were inseminated using epididymal frozen semen in IVF medium modified Pig-FM supplemented with 2 mM caffeine and 5 mg mL–1 bovine serum albumin (Kikuchi et al. 2002). The percentage of cleaved embryos and percentage of cleaved embryos which developed to the compact morula and early blastocyst stage were recorded. Results were analysed by one-way ANOVA followed by Dunnett’s test. To investigate the effects of co-culture with mouse embryonic fibroblasts and oviduct epithelial cells on oocyte maturation, some COCs cultured in groups 1, 2, 5, and 8 were fixed to assess their nuclear maturation to the metaphase II stage. The rate of matured oocytes in the groups 2, 5, and 8 was 76.85 ± 3.39% (n = 102), 79.11 ± 3.75% (n = 64), and 81.84 ± 3.93% (n = 66), respectively; these rates were increased significantly compared to the group 1 (55.87 ± 1.88%, n = 94; P < 0.05). The effect of co-culture on the fertilization and embryo development is shown in Table 1. Our results indicate that co-culture increases the rates of embryonic cleavage in all groups by comparison with the control group. However, a significant increase in the rate of morula-blastocyst was only observed when embryos were co-cultured with fibroblasts or when both maturation and culture were performed in co-culture with either fibroblasts or oviduct cells (groups 3, 4, 7, and 8). The most important increase in morula-blastocyst rate was recorded for the group of embryos co-cultured with fibroblasts (group 3). In conclusion, the co-culture with fibroblast or oviduct cells during maturation can improve oocyte maturation and cleavage rate, while co-culturing the embryos with fibroblasts seems sufficient to improve both the cleavage and the morula-blastocyst rates. Table 1.Effect of co-culture on the fertilization and embryo development in pig Supported by a grant from the NAFOSTED VN.

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Grigg, Andrew H. "LITTER DECOMPOSITION ON DIRECTLY REVEGETATED TAILINGS AT THE KIDSTON GOLD MINE, NORTH QUEENSLAND, AUSTRALIA." Journal American Society of Mining and Reclamation 2002, no. 1 (June 30, 2002): 708–24. http://dx.doi.org/10.21000/jasmr02010708.

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Edraki, Mansour, Thomas Baumgartl, David Mulligan, Warwick Fegan, and Ali Munawar. "Geochemical characteristics of rehabilitated tailings and associated seepages at Kidston gold mine, Queensland, Australia." International Journal of Mining, Reclamation and Environment 33, no. 2 (August 23, 2017): 133–47. http://dx.doi.org/10.1080/17480930.2017.1362542.

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