39 research outputs found
A Juridical Study toward Indonesian Disabilities Right for Public Services Accessibility according to Law No. 8 Year 2016
No full textIn this study, the author is very attentive to law for disability. In 2016, the Indonesian government has been launched a recovering law for persons with disabilities, namely Law No. 8 Year 2016. Differ with the previous law, Law No. 4 Year 1997 which still less contains the rights of persons with disabilities, especially on the things of public services accessibility. Hence, regarding to the normative analysis toward Law No. 8 Year 2016 which is used in this study. It found that the Indonesian government is already loaded the persons with disabilities right on public services accessibility. Those listed in Chapter III, Part 15 article 19 on Public Service Rights. Therefore, the development of public service facility for persons with disabilities shall be appropriate to this law. Furthermore, the details of public service in terms of implementation of respect, protection and rights meeting with disabilities are initiated by both central and local governments. All public services in Indonesia should be take attention to the Law No. 8 Year 2016 on Persons with Disabilities
Exploring the Accessibility and Facility in Railway Station Used by Persons With Disabilities: an Experience From Kebayoran Railway Station, Jakarta
No full textThis paper discusses accessibility at Kebayoran Railway Station's facility for persons with disabilities. Kebayoran Railway Station as one of Railway Stations on Tanah Abang, Rangkasbitung railway track, which has been revitalized in 2016. A descriptive approach used in this research and found that currently, Kebayoran Railway Station has been more accessible for persons with disabilities. The results indicate that some disability's facilities consist of: (a) toilet; (b) safe pick-up and set-down facility; (c) facility for persons with disability; (d) other facility (tactile paving). The Minister of Transportation Decree 47 Year 2014 regarding Minimum Service Standard for Train Public Transportation at Kebayoran Railway Station facilities is one of the guidelines for PT. KAI Commuter Jabodetabek in building facilities in the station. In this case, Kebayoran Railway Station has implemented the Minister of Transportation's Decree and makes it easy for some persons with disabilities to use the facilities at the railway station
Aksesibilitas Sarana dan Prasarana bagi Penyandang Tunadaksa di Universitas Brawijaya
No full textThe provision of good accessibility of infrastructure facilities is the main duty of an institution to become an institution that is good for all parties. However, problems frequently arise is still the lack of infrastructure that is less accessible for the disabled. The University of Brawijaya as an institution of higher education higher based inclusive prompted many changes to the accessibility infrastructure that is friendly to people with disabilities, especially physical disabilities (ambulant disabled and. This paper aims to find the accessibility of facilities in the UB for a physical disabled people. With an emphasis on means of pedestrian, doors, lifts, ramps and toilets at some points in UB faculties and buildings
Jurassic accretionary complex of the Tamba Terrane, Southwest Japan and its formative process
No full textRancang Sistem Absensi Siswa menggunakan ID Card dengan Pemberitahuan SMS Berbasis Mikrokontroller At Mega 16.
No full textThe system of Radio frequency identification (RFID) is a technology that uses
communication via electromagnetic waves to change data between terminals with
an object such as product goods, animals, or humans with the aim to Here the
author uses identification identification is a STUDENT ID CARD and searches
the trail through the use of a device called the RFID tag. RFID tags can be active
or passive. Passive RFID tags do not have their own power supply, so the price is
cheaper than active tags. Where the later process when On the RFID reader is
going to read RFID tags on your STUDENT ID CARD, ID expected in reading
will be stored in EEPROM and will be compared with the existing STUDENT ID
at the student information system to send messages to the presence use the
MODEM WAVE COM to parents of students.53 HalamanSkripsi Sarjan
Perancangan alat pendeteksi jarak aman mobil menggunakan sensor ultrasonik dengan output suara berbasis mikrokontroler atmega328p
No full textVehicle safety distance detection monitoring system has a very important role in human life. Especially when driving or going to park a vehicle. with this tool the driver can help estimate a safe distance on the vehicle. In this thesis the author uses an ultrasonic sensor as a tool to detect distance, and IC LM7809 as a voltage amplifier with Arduino as its control center that is able to display the distance readable by the sensor on a 16x2 LCD and is equipped with LEDs and buzzers and sound modules as additional displays. From the results of testing the prototype hardware and software safe distance detection tool, the tool works well and has an average reading error of only one cm difference with the actual distanceSistem monitoring deteksi jarak aman kendaraan mempunyai peranan yang sangat penting dalam kehidupan manusia. Terutama saat berkendara maupun sedang akan memarkirkan kendaraan. dengan alat ini pengendara dapat terbantu memperkirakan jarak yang aman pada kendaraanya. Dalam tugas akhir ini penulis menggunakan sensor ultrasonik sebagai alat untuk mendeteksi jarak, dan IC LM7809 sebagai penguat tegangannya dengan Arduino sebagai pusat kendalinya yang mampu menampilkan jarak yang terbaca oleh sensor pada LCD 16x2 dan dilengkapi dengan LED dan Buzzer dan modul suara sebagai display tambahan. Dari hasil pengujian hardware dan software prototype Alat deteksi jarak aman, alat berfungsi dengan baik dan mempunyai rata- rata kesalahan pembacaan hanya selisih satu cm dengan jarak actual63 HalamanKertas Karya Diplom
Rancang Bangun Alat Pendeteksi Asap Rokok Berbasis Arduino Nano dengan Menggunakan Smartphone Android
No full textKurangnya fasilitas ruangan untuk para perokok juga kurang memadai seperti tidak
adanya pembersih udara pada ruangan khusus perokok sehingga menimbulkan asap
yang mengendap pada ruangan. Oleh karena itu penulis telah merancang dan
merealisasikan sebuah perangkat yang dapat mendeteksi asap rokok dan kemudian
menetralisirkannya, alat ini nantinya berfungsi untuk mengeluarkan asap rokok yang
terperangkap pada ruangan khusus merokok dan mengubahnya menjadi ruangan
bebas asap rokok. Perancangan ini dikontrol menggunakan mikrokontroller arduino
nano sebagai pusat dari seluruh pengendalian sistem yang dapat menampilkan hasil
dari kadar asap yang terdeteksi oleh sensor MQ2 pada layar LCD. Kemudian
mikrokontroller ini akan memerintahkan driver untuk mengaktifkan output pada alat
ini berupa aktifasi fan. Alat ini diprogram memiliki dua keadaan. Keadaan pertama
jika sampai 80 ppm (kadar asap) makan fan akan mati. Keadaan kedua jika sampai
200 ppm atau lebih maka fan akan menyala. Berdasarkan hasil pengujian alat ini
mampu mendeteksi kadar asap rokok yang terkumpul pada suatu ruangan dengan
baik, dan membutuhkan waktu beberapa saat untuk menetralisirkan ruangan yang
terkontaminasi asap rokok menjadi ruangan bebas asap rokok.The lack of room facilities for smokers is also inadequate, such as the absence of air
purifiers in special smoker rooms, causing smoke to settle in the room. Therefore the
author has designed and realized a device that can detect cigarette smoke and then
neutralize it, this tool will later function to remove cigarette smoke trapped in a
smoking room and turn it into a smoke-free room. This design is controlled using the
Arduino Nano microcontroller as the center of all system controls that can display
the results of the smoke levels detected by the MQ2 sensor on the LCD screen. Then
this microcontroller will instruct the driver to activate the output on this tool in the
form of fan activation. This tool is programmed to have two conditions. The first
situation if up to 80 ppm (smoke content) eat the fan will die. The second situation if
it reaches 200 ppm or more, the fan will turn on. Based on the results of testing this
tool is able to detect the level of cigarette smoke collected in a room properly, and it
takes a few moments to neutralize the room contaminated with cigarette smoke into a
smoke-free room.56 HalamanSkripsi Sarjan
The Relationship Between the EU Charter and the ECHR in the EU and the EEA. The Level of Protection Afforded in the EU Post Lisbon and Pre Accession by the EU to the ECHR
No full textThe objective of this thesis is twofold; partly it is to present the factors that define and affect the relationship between these fundamental rights in the EU and in the EEA Area on a European level (Chapter 2); partly it is to highlight the differences in protection guaranteed under each catalogue (Chapter 3). In the process the author hopes to provide grounds for further thought and consideration on this subject
Rancang Bangun Alat Ukur Konsentrasi Karbon Dioksida (CO2) pada Ruangan Berbasis Arduino dengan Sensor MQ135
No full textCarbon dioxide is an important part of the air, and every human being desperately needs air in the breathing process, but we do not know what level of carbon dioxide (CO2) in the air we need. Hence the need to monitor the levels of carbon dioxide (CO2) in the air with a concentration measuring instrument levels of carbon dioxide (CO2) -based sensor arduino with MQ-135, with this measure we can determine the level of concentration of carbon dioxide (CO2) using MQ- 135 as the sensor levels of carbon dioxide (CO2) and san, base arduino as a microcontroller that has been in the program that can meproses content level of carbon dioxide (CO2) in the air. Output output or output of the levels of carbon dioxide (CO2) will be in tampailkan on the LCD. With this tool we can easily determine the level of concentration of carbon dioxide (CO2) in a region or in a room and can cope with it if tingakat this gas exceeds a predetermined threshold. With this tool the author can implement one project as one of the parameters graduation.Karbon dioksida merupakan bagian penting dari udara, dan setiap manusia sangat membutuhkan udara dalam proses bernapas, namun kita tidak mengetahui berapa tingkat karbon dioksida (CO2) dalam udara yang kita butuhkan. Maka dari itu dengan perlu monitoring kadar karbon dioksida (CO2) di udara dengan alat ukur konsentrasi kadar karbon dioksida (CO2) berbasis arduino dengan sensor MQ-135, dengan alat ukur ini kita dapat mengetahui tingkat kadar karbon dioksida (CO2) dengan menggunakan MQ-135 sebagai sensor tingkat karbon dioksida (CO2) dan san, basis arduino sebagai mikrokontroler yang sudah di program yang dapat meproses tingkat kadar karbon dioksida (CO2) di udara. Output output atau keluaran dari pada tingkat karbon dioksida (CO2) akan di tampailkan pada LCD. Dengan alat ini kita dengan mudah mengetahui tingkat kadar karbon dioksida (CO2) pada suatu daerah atau pun dalam suatu ruangan dan dapat menanggulangi nya jika tingakat gas ini melebihi amabang batas yang telah ditentukan. Dengan alat ini penulis dapat melaksanakan proyek 1 sebagai salah satu parameter kelulusan mahasiswa.Kertas Karya Diplom
西南日本内帯西部地域における中・古生代造構作用の研究
No full textThe Upper Paleozoic - Lower Mesozoic sequences widely develop in the Inner Zone of Southwest Japan just on the south of the Hida belt. Most of them are considered to be accretionary complexes formed in consuming plate-boundaries during Middle Permian to Late Jurassic age. In this paper the author has attempted to clarify evolutional proceses of those accretionary complexes.
The western half of the Inner Zone of Southwest Japan consists of the Chugoku - Maizuru belt and Tamba belt. The fundamental tectono-stratigraphic subunits of the Chuoku - Maizuru belt are classified as followes: 1) High-P/T type metamorphic rocks ("Sangun metamorphic rocks"). This subunit is further divided into several subgroups as described in later paragraph. 2) Non-metamorphic Paleozoic formations. This subunit is further divided into two subgroups following Hase(1964). (a) North zone Paleozoic formations as a Late Permian accretionary prism cosisting mainly of seamount - reaf-limestone complexes such as Akiyoshi, Taishaku and Atetsu chert -limestone - greenstone complexes, clastic rocks and acidic tuff. (b) Middle zone Paleozoic formations and maizuru group in the Maizuru belt as a Late Permian accretionary prism consisting mainly of Yakuno rocks and clastic rocks with subordinate acidic tuff and hemipelagic reddish-claystone. 3) Equivalents of theTamba group in the Tamba belt: Middle to Latest Jurassic accretionary coplexes consisting mainly of bedded chert, siliceous claystone, pebbly mudstone and greenstones with sub-ordinate limestone lenses. 4) Triassic and Jurassic formations of blackish to shallow water facies: subunit consisting mainly of relatively coarse-grained clastic rocks. They unconformably overlie the non-metamorphic Paleozoic formations. 5) Ultra Tamba zone (Ishiga, 1985; Caridroit et al., 1985) as a Triassic (probably) accretionary complex developed between the Maizuru belt and the Tamba belt.
The author has clarified that the Chugoku belt is divided into two units, NE unit and SW unit, by a narrow zone which cuts across the general distribution trend of the above-mentioned constituent subunits of the Chugoku blet from the Nichihara - Tsuwano district to the North of Hiroshima and consists of the equivalents of the Tamba group. The two units are different from each other mainly with respec to some important characteristics of the "Sangun metamorphic rocks": a) distribution trend of metamorphic rocks (Fig. 1), b) orientation trend of mineral lineations (Fig. 4), c) original rock assemblage (Fig. 5), d) radiometric age (Fig. 6), e) distribution frequency of lawso-nite-bearing schist (frequently found in the NE unit, but only one lacality in the SW unit), and f) volume of Yakuno rocks (abundant in the weekly metamorphosed Paleozic formations of the NE unit, but rare in those of the SW unit). Because Paleozoic formation of the Northern zone of the NE unit has essentially the same property as that of the SW unit, the author has pointed out that those two units appeared after the formation of the Paleozoic formation.
Recently, the radiometric age of "Sangun metamorphic rocks" has extensively been measured mainly by Shibata and Nishimura(1983, 1984, 1985), showing that the "Sangun metamorphic rocks" of the Northern district of the Chugoku belt are of 280 - 310 Ma, those of the Western district of 210 - 220 Ma and those of the Eastern district of 170 - 190 Ma (Fig. 6). The Northern district corresponds to the northern margin of the Chugoku belt (NE unit and SW unit), while the Western and the Eastern district correspond to the remaining part of the SW unit, and to that of the NE unit respectively. Metamorphic rocks of the Northern district are correlated with those of the Hida marginal belt. The author has found some fossiles such as Triassic Conodonts and Early Jurassic Radiolarians and high-P/T type minerals such as alkali and sodic-calcic amphiboles (Table 2) and lawsonites (Table 3), from the Hatto formation in the Mochigase district, Tottori Prefecture (Table 1), which has been considered to be a member of the "Sangun metamorphic rocks", showing that in the Chugoku zone there are Jurassic high-P/T type metamorphic sequences. Original rock assemblage of the Hatto formation consists mainly of bedded chert, greenstone, siliceous claystone and pebbly mudstone, being comparable with that of the Type II suite formations of the Tamba group which are of Jurassic age. The "Sangun metamorphic rocks" with such original rock assemblage are found only in the NE unit (Fig. 12), forming relatively low-grade metamorphic portion of them and commonly associating the equivalents of the Tamba group. Other "Sangun metamorphic rocks" in the NE unit, which consist mainly of elastic rocks and greenstones with subordinate limestones, are closely associated with the non-metamorphic Paleozoic formations. On the other hand the metamorphic rocks of the SW unit may form a unique tectono-stratigraphic subunit.
The author has studied the geology of the Maizuru zone of the Asako-cho district, Hyogo Prefecture, showing that the border zone between the Maizuru and the Tamba belt is structurally characterized by a pile nappe structure consisting of nappe of the Tamba groupe, nappe of the Ultra Tamba zone and three nappes of Yakuno rocks, and that the Yakuno rocks were produced by igneous activities of two stages. The first-stage Yakuno rocks form a pseudostratiform sequence, containning Pyroxenite member, Transitional zone, Lower Gabbro member, Upper Gabbro member and Dolerite member in ascending order, and correspond to the Yakuno ophiolite after Ishiwatari(1978). The second-stage Yakuno rocks consist mainly of tonalite and quartz-diorite, which discordantly intruded the first-stage Yakuno rocks. The constituent minerals such as clinopy-roxenes of the Lower Gabbro memger and amphiboles of the Upper Gabbro member of the first-stage Yakuno rocks have preferred lattice orientation, showing their metamorphic nature (Figs. 18, 19). The maximum Ti content of such metamorphic amphiboles increases towards the lowest horizon of the volcano-plutonic sequence, shwing increase of metamorphic grade from the greenshcist facies in the upper part of the Dolerite member to the hornblende-granulite facies of the lowest part of the Lower Gabbro member and the Pyroxenite member (Fig. 21). Such metamorphism may be ascribed to sea floor metamorphism accomplished before dismembering of the ophiolitic sequence of the first-stage Yakuno rocks. With referece to major element chemistry of whole rock and phenocryst clinopyroxene, it may be said tha the first-stage Yakuno rocks are comparable with either some E-type MORB or tholeiite of ocean plateau with relatively thick crust (Fig. 26). On the ohter hand, the second-stage Yakuno rocks appear to be regarded as arc-related igneous rocks (Fig. 24). It has been also pointed out that the greenstones of the Chugoku and Tamba belts associated with bedded cherts are commonly of seamount, ocean island and/or ocean plateau (Fig. 27). MnO/TiO 2 vs MnO/Al2O3 plots of the Triassic beded cherts of the Mino belt also sugest a possibility that they were produced in pelagic but relatively shallower environments such as ocean plateau, seamount or flank of ocean island (Fig. 30).
Thus the tectonic developement of the Chugoku, Maizuru and Tamba belts during Carboniferous to Jurassic age has been synthesized as below.
1) Early Carboniferous to Early Permian age
During Early Carboniferous age, on a sea floor (Akiyoshi ocean floor) appeared seamounts with reef-limestone complexes of Hiraodai, Akiyoshi, Taishaku, Atetsu and Omi. All rocks arround them deposited during this age was of pelagic type. During Late Carboniferous age, subduction of the Akiyoshi coean floor began at the front of the Hida - Hida marginal belt.
2) Middle to Late Permian age
Accretionary prisms of non-metamorphic Paleozoic formations related to the subduction of the Akiyoshi ocean floor had not began to form untill Middle Permian age, and their formation appears to have ceased during Latest Permian age. During this period, either T-T-R type or R-F-T type triple-junction arrived at the front of the Hida - Hida marginal belt, forming the first-stage Yakuno rocks (the Yakuno ophiolite) together with sedimentation of fine-grained terrigenous materials. This was followed by collision of young aseismic ridge. After this collision, the trench and vol-canic front were sifted oceanward. Hence, the collided first-stage Yakuno rocks were involved in arc-related igneous activities, forming the second-stage Yakuno rocks.
3) Triassic age
Because any volcanic activity has not been known throughout the Hida - Chugoku - Maizuru belt, it has been inferred that, after passing away of the tripple-junction, the subduction ceased during Early to Middle Triassic age. While acidic tuffs of small amount are found in the Upper Triassic formation, although their petrologic characteristics have not yet been clarified. Thus it seems probable that during Late Triassic age the plate boundary had turned into of highly oblique subduction, forming the accretion of rocks of the Ultra Tamba zone.
4) Jurassic age
During Early Jurassic age were produced such "Sangun metamorphic rocks" as the Hatto formation with high-P/T minerals, followed by a volumenous accretion of Type II suite formation of the Tamba belt during Middle Jurassic age. During the Latest Jrassic age, the Type I suite formation of the Tamba group had underthrusted bnenerth the Permian to Jurassic complexes of the Chugoku blet, forming a pile-nappe structure of the Chugoku and Tamba belts. The Early Cretaceous arc-volcanisms widely occured in these belts as a tectonic collage.
It has been clarified that, althogh the formation of the Chugoku and Tamba belts is ascribed to acrretion tectonics, any constituent material of normal type abyssal plane such as N-type MORB or typical pelagic sediment is not involved in the constituent rocks of those belts and they commonly contain oceanic materials derived from topographically prominent highs on oceanic plate such as seamount, ocean island and/or ocean plateau. This fact strongly suggests that only the collision of the seamount, ocean island and/or ocean plateau during Permian to Jurassic age was responsible for the formation of accretion complexes of the Chugoku and Tamba belts.Doctoral thesis（Science）submitted to Hiroshima University in 1986
