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Journal articles on the topic 'Godeaux surface'

Author: Grafiati

Published: 14 March 2023

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1

Werner, Caryn. "A four-dimensional deformation of a numerical Godeaux surface." Transactions of the American Mathematical Society 349, no. 4 (1997): 1515–25. http://dx.doi.org/10.1090/s0002-9947-97-01892-8.

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2

Böhning, Christian, Hans-Christian Graf von Bothmer, and Pawel Sosna. "On the derived category of the classical Godeaux surface." Advances in Mathematics 243 (August 2013): 203–31. http://dx.doi.org/10.1016/j.aim.2013.04.017.

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3

Murakami, Masaaki. "The torsion group of a certain numerical Godeaux surface." Journal of Mathematics of Kyoto University 41, no. 2 (2001): 323–33. http://dx.doi.org/10.1215/kjm/1250517636.

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4

KEUM, JONGHAE, and YONGNAM LEE. "Fixed locus of an involution acting on a Godeaux surface." Mathematical Proceedings of the Cambridge Philosophical Society 129, no. 2 (September 2000): 205–16. http://dx.doi.org/10.1017/s0305004100004497.

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5

Franciosi, Marco, Rita Pardini, and Sönke Rollenske. "Gorenstein stable Godeaux surfaces." Selecta Mathematica 24, no. 4 (July 7, 2017): 3349–79. http://dx.doi.org/10.1007/s00029-017-0342-6.

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6

Liedtke, Christian. "Non-classical Godeaux surfaces." Mathematische Annalen 343, no. 3 (September 13, 2008): 623–37. http://dx.doi.org/10.1007/s00208-008-0284-6.

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7

Calabri, Alberto, Ciro Ciliberto, and Margarida Mendes Lopes. "Numerical Godeaux surfaces with an involution." Transactions of the American Mathematical Society 359, no. 04 (October 17, 2006): 1605–33. http://dx.doi.org/10.1090/s0002-9947-06-04110-9.

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8

Franciosi, Marco, and Sönke Rollenske. "Canonical rings of Gorenstein stable Godeaux surfaces." Bollettino dell'Unione Matematica Italiana 11, no. 1 (January 5, 2017): 75–91. http://dx.doi.org/10.1007/s40574-016-0114-9.

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9

Coughlan, Stephen, and Giancarlo Urzúa. "On $\boldsymbol{{\mathbb Z}/3}$-Godeaux Surfaces." International Mathematics Research Notices 2018, no. 18 (March 20, 2017): 5609–37. http://dx.doi.org/10.1093/imrn/rnx049.

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10

Coughlan, Stephen. "EXTENDING HYPERELLIPTIC K3 SURFACES, AND GODEAUX SURFACES WITH π1= ℤ/2." Journal of the Korean Mathematical Society 53, no. 4 (July 1, 2016): 869–93. http://dx.doi.org/10.4134/jkms.j150307.

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11

Kim, Soonyoung. "Numerical Godeaux surfaces with an involution in positive characteristic." Proceedings of the Japan Academy, Series A, Mathematical Sciences 90, no. 8 (August 2014): 113–18. http://dx.doi.org/10.3792/pjaa.90.113.

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12

Kulikov, Vik S. "On divisors of small canonical degree on Godeaux surfaces." Sbornik: Mathematics 209, no. 8 (August 2018): 1155–63. http://dx.doi.org/10.1070/sm9032.

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13

Lee, Yongnam. "A compactification of a family of determinantal Godeaux surfaces." Transactions of the American Mathematical Society 352, no. 11 (June 13, 2000): 5013–23. http://dx.doi.org/10.1090/s0002-9947-00-02393-x.

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14

KOTSCHICK, D. "ON THE PLURICANONICAL MAPS OF GODEAUX AND CAMPEDELLI SURFACES." International Journal of Mathematics 05, no. 01 (February 1994): 53–60. http://dx.doi.org/10.1142/s0129167x94000036.

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15

Lee, Yongnam. "Semistable Degeneration of Godeaux Surfaces with Relatively Nef Canonical Bundle." Mathematische Nachrichten 219, no. 1 (November 2000): 135–46. http://dx.doi.org/10.1002/1522-2616(200011)219:1<135::aid-mana135>3.0.co;2-5.

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16

Rollenske, Sönke. "A new irreducible component of the moduli space of stable Godeaux surfaces." Manuscripta Mathematica 149, no. 1-2 (July 28, 2015): 117–30. http://dx.doi.org/10.1007/s00229-015-0776-0.

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17

Iqbal, Sohail. "Godeaux, Campedelli, and surfaces of general type with χ=4 and 2≤K2≤8." Mathematische Nachrichten 290, no. 14-15 (March 29, 2017): 2296–307. http://dx.doi.org/10.1002/mana.201500445.

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18

Hartono, Hill Gendoet, Adjat Sudradjat, and Okki Verdiansyah. "Caldera of Godean, Sleman, Yogyakarta: A Volcanic Geomorphology Review." Forum Geografi 31, no. 1 (July 1, 2017): 138–47. http://dx.doi.org/10.23917/forgeo.v31i1.2821.

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Godean hills is located approximately 10 km westward from the Yogyakarta City. The landscape of Godean hills and plains is affected by various factors, such as lithology, geological structure, and sub-aerial process. The purpose of this study was to reveal the landscape of Godean. The method consisted of field study, morphological variables assessment, rock sampling, and laboratory analysis. The results of field mapping indicated that the landscape of Godean is an isolated hill with a steep slope of >40° and an elevation of +231 m a.s.l, passed by the rivers flows from northeast to southwest that disembogue into the west part of Kulon Progo. The morphologhy of Godean hills varies including G. (Gunung/Mountain) So (+173 m amsl), G. Gede (+218 m a.s.l), G. Wungkal (+187 m a.s.l), G. Butak (+154 m a.s.l), and G. Berjo ( + 175 m a.s.l), dominated by the lithology of igneous rock, which is composed of porphyry andesite-microdiorite, pumice lapilli, and quartz rich lapilli-tuff. In addition, most of the igneous rocks have weathered and have been altered to clays, while the deposition from Merapi volcano formed a landscape with an altitude between +100–+150 m a.s.l surrounding Godean hills. Sentolo Formation was found in Kembang, Bantul, which is located approximately ±5km in the south of the study area N93ºE/12º, while the distribution in the southwest and northeast relatively covers the Godean hills in curve shape. The results of the analysis provide information related with Godean landscape that it is the remains of the volcanic caldera, with various igneous rock types and volcaniclastics deposits, as well as endured the occurrences of hydrothermal alteration and mineralization. Further geophysical research is required to determine the configuration of igneous rocks under the earth's surface.

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19

Khairudin, Jati, Adib Suyanto, and Sigid Sudaryanto. "Pemberian Variasi Model Alat Pemungut Sampah Terhadap Frekuensi Memungut Sampah Murid TK Kudup Sari di Sidoluhur, Godean, Sleman, Tahun 2016." Sanitasi: Jurnal Kesehatan Lingkungan 8, no. 1 (May 15, 2016): 9–15. http://dx.doi.org/10.29238/sanitasi.v8i1.732.

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Waste management can involve the entire community, including children. The involvement of very young children is a good first step for them to learn how to handle waste and to be respon-sible for caring the environment. The average age of Kudup Sari Kindergarten’s students, which is located in Sidoluhur, Godean, Sleman, is 6 years old. Children at this age are in the stage of imitating and receiving new knowledge easily. Therefore, it is expected that the children can easily apply the new received knowledge. This study was aimed to reveal the most preferred model of trash picking device among kindergarten children by conducting a quasi experiment which employed post-test only design. The population and sample of the study were all 41 stu-dents in the Class B of Kudup Sari Kindergarten. The observation was held in 10 times to ob-serve the number of children who pick the trash up that using the two picking models. Des-criptively, the difference of frequency average of trash picking is obvious, i.e. 4 times with the piercing model against 37 times with the clipping model. The result of independent t-test at 95 % level of confidence confirmed the difference since the obtained p-value that was smaller than 0,001, showing a significant disparity between the two averages. Therefore, this study shows that the clipping model is much more preferred by Kudup Sari Kindergarten students to pick trash than the piercing one.

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20

Purwanto, Taufik Hery. "Pemanfaatan Foto Udara Format Kecil untuk Ekstraksi Digital Elevation Model dengan Metode Stereoplotting." Majalah Geografi Indonesia 31, no. 1 (April 21, 2017): 73. http://dx.doi.org/10.22146/mgi.24246.

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Perkembangan Unmanned Aerial Vehicle (UAV) sebagai wahana dan kamera digital non-metrik sebagai sensor semakin mempermudah dalam akuisisi data foto udara Foto Udara Format Kecil (FUFK). Penelitian ini bertujuan menerapkan metode stereoplotting digital untuk menghasilkan Digital Elevation Model (DEM) dari FUFK hasil pemotretan udara dengan wahana UAV sebagian bukit Jering yang merupakan lokasi pembangunan perumahan murah bersubsidi Godean Jogja Hill’s. Metode penelitian ini meliputi: proses perencanaan (perencanaan jalur terbang, pelaksanaan pemotretan udara), pengolahan data (kalibrasi kamera, koreksi foto udara, stereoplotting, interpolasi), dan uji akurasi. Hasil penelitian adalah blok FUFK dan DEM dengan metode stereoplotting. Kesimpulan dari penelitian ini adalah FUFK yang diperoleh dari UAV memiliki distorsi lensa yang cukup besar, oleh karena itu stereoplotting interaktif dapat diterapkan pada FUFK dengan hasil yang cukup baik jika FUFK yang digunakan telah terkoreksi dari distorsi, terutama distorsi lensa. Akurasi absolut DEM yang dihasilkan memiliki HRMSE sebesar 0.073 meter dengan horizontal accuracy yang mencapai 0.121 meter, sedangkan RMSEz yang dimiliki hanya mampu mencapai 0.482 meter dengan vertical accurasi yang mencapai 0.793 meter pada tingkat kepercayaan 90%. Berdasarkan DEM yang diperoleh, maka dapat digunakan untuk merepresentasikan konfigurasi permukaan bukit dan menghitung volume sebagian bukit Jering yang telah dikeruk sebesar 55.953,813 m3. The development of Unmanned Aerial Vehicle (UAV) as a vehicle and non-metric digital camera as a sensor further simplify the data acquisition of Small Format Aerial Photography (SFAP). This study aims to apply digital stereoplotting method for generating Digital Elevation Model (DEM) of SFAP results of aerial photography with UAV on the Jering hill which is cheap subsidized housing location named Godean Yogyakarta Hill’s. This research method includes: flight planning (flight paths, aerial photography acquisition), data processing (camera calibration, correction of aerial photographs, stereoplotting, interpolation), and accuracy test. Results of the research was SFAP block and DEM generated from stereoplotting method. The conclusion of this study is SFAP obtained from UAV has a lens distortion is large, and therefore can be applied to interactive stereoplotting SFAP with fairly good results if SFAP used has been corrected of distortion, especially distortion lens (idealized). The absolute accuracy of the resulting DEM have HRMSE of 0,073 meters with a horizontal accuracy which reaches 0,121 meters, while RMSEz only able to reach 0,482 meters with a vertical accuracy which reaches 0793 meters at 90% confidence level. Based on the DEM obtained, it can be used to represent the surface configuration and to calculate the volume partially Jering hill that has been dredged out for is 55.953,813 m3.

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21

Alexandrou, Theodosis. "On the Brauer group of a generic Godeaux surface." Journal of the London Mathematical Society, February 15, 2023. http://dx.doi.org/10.1112/jlms.12727.

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22

Schreyer, Frank-Olaf, and Isabel Stenger. "An 8-dimensional family of simply connected Godeaux surfaces." Transactions of the American Mathematical Society, February 3, 2023. http://dx.doi.org/10.1090/tran/8813.

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In this paper we describe a construction method for numerical Godeaux surfaces based on homological algebra. We show the existence of an 8-dimensional locally complete family of simply connected numerical Godeaux surfaces.

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23

Fantechi, Barbara, Marco Franciosi, and Rita Pardini. "Smoothing semi-smooth stable Godeaux surfaces." Algebraic Geometry, July 1, 2022, 502–12. http://dx.doi.org/10.14231/ag-2022-015.

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24

Palmieri, Eleonora. "Automorphisms of order three on numerical Godeaux surfaces." ANNALI SCUOLA NORMALE SUPERIORE - CLASSE DI SCIENZE, May 4, 2009, 483–543. http://dx.doi.org/10.2422/2036-2145.2008.3.05.

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25

Dias, Eduardo, Carlos Rito, and Giancarlo Urzúa. "On degenerations of $\mathbb{Z}/2$-Godeaux surfaces." Revista Matemática Iberoamericana, August 31, 2022. http://dx.doi.org/10.4171/rmi/1376.

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