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Bayangkan diri Anda jauh ke tengah laut, ada daratan di depan mata, berlayar dalam sebuah kapal kecil. Pada siang hari, navigasi Anda oleh matahari dan pada malam hari oleh bintang-bintang. Kemudian menjadi mendung selama beberapa hari yang panjang. Saya berani bertaruh Anda pasti ingin memiliki sebuah kompas...
Sifat magnetik menarik lodestone(batu magnet), mineral yang dikenal sebagai magnetit (Fe 3 O 4) ahli geologi, telah dikenal sejak zaman Yunani kuno. Itu tidak sampai beberapa abad kemudian ketika pelaut di Cina (dan pada abad ke-12, pelaut di Eropa) menyadari bahwa sepotong lodestone, ketika pada sebatang tongkat mengambang dalam mangkuk air, menyejajarkan diri untuk menunjuk ke arah bintang utara. Ini adalah penemuan yang merevolusi dunia karena memungkinkan untuk meningkatkan navigasi pelayaran dan penjelajahan. Penemuan yang sederhana ini telah dikembangkan, dari waktu ke waktu, menjadi kompas modern.
Kompas bekerja karena bumi bertindak seperti magnet batang raksasa. Gerakan dalam inti besi-nikel, cair bumi menginduksi medan magnet dengan kutub utara dan selatan. Garis gaya magnetik menghubungkan sebelah utara Bumi dan selatan kutub magnet menunjukkan sebagai berikut:
Kompas bekerja karena jarum magnet kompas akan menyesuaikan diri dengan garis-garis magnetik bumi dengan kekuatan dan titik di sekitar utara. Saya mengatakan ada di sekitar karena Anda akan perhatikan pada gambar di atas bahwa kutub utara dan selatan magnet tidak persis sejajar dengan sumbu rotasi bumi yang mendefinisikan geografis utara dan kutub selatan.
Ahli geologi struktural menggunakan kompas untuk membuat peta geologi dan mengukur orientasi struktur geologi. Oleh karena itu, dalam rangka untuk melakukan penelitian struktur geologi di lapangan, Anda perlu tahu bagaimana kompas bekerja dan bagaimana menggunakannya dengan benar satu.
Azimuths vs Quadrants
Ada tiga cara yang umum untuk menyatakan arah dengan kompas. Yang pertama adalah hanya untuk memperkirakan arah Anda sebagai utara, timur, selatan, atau barat. Jika Anda ingin sedikit lebih presisi, Anda dapat menggunakan timur laut, barat laut, tenggara, atau juga barat daya. Untuk tujuan ini, kompas di bawah ini akan bekerja dengan baik.
Mari kita luangkan waktu untuk memastikan kita memahami bagaimana kompas tersebut bekerja. Apakah Anda tahu mengapa, misalnya, bahwa E (timur) dan W (barat) muncul terbalik di kompas di atas?
Jarum kompas magnetik dan menyelaraskan diri dengan medan magnet bumi sehingga ujung putih jarum menunjuk ke arah kutub magnet utara. Mari kita memegang sebuah kompas sementara kita menghadap utara. Panah dan N pada kompas akan berbaris seperti gambar di bawah di sebelah kiri.
Sekarang mari kita berbalik dan menghadap timur laut(northeast). Jarum kompas tidak bergerak, dia selalu menunjuk ke utara, dan sekarang letaknya setengah jalan antara N dan E (timur laut) pada kompas. Mari kita terus berbalik dan muka timur. Jarum kompas masih menunjuk ke arah utara tapi sekarang garis dengan E pada kompas menunjukkan bahwa kita menghadap ke timur. Lihat mengapa E dan W di muka kompas dibalik?
Sementara kompas tersebut mungkin baik untuk casual hiking, itu jelas sangat tidak tepat dan orang-orang yang melakukan pengukuran (seperti ahli geologi struktural) perlu memiliki data yang lebih akurat. Kompas yang digunakan oleh ahli geologi struktural biasanya datang dalam dua bentuk - mereka yang menggunakan notasi azimut dan mereka yang menggunakan notasi kuadran. Mari kita periksa masing-masing pada gilirannya ...
Dalam notasi azimut, lingkaran dibagi dari 0 ° sampai 359 ° searah jarum jam. Utara berada 0 °, timur adalah 90 °, selatan adalah 180 °, dan barat adalah 270°.
Dalam memindahkan ini ke muka sebuah kompas, angka meningkat dari 0 ° sampai 359 ° dalam arah berlawanan jarum jam (untuk tetap konsisten dengan pembalikan E dan W pada kompas).
Ini disebut notasi azimut. Jika Anda menghadap ke timur, Anda akan mengatakan bahwa azimuth adalah 90 °. Jika Anda menghadap ke selatan, Anda akan mengatakan bahwa azimuth adalah 180 °.
Sekali lagi, dalam notasi azimut, arah Anda ditetapkan sebagai sudut antara 0 ° dan 359 ° dimana utara(north) adalah 0 °, timur(east) dalam 90 ° , selatan(south) adalah 180 °, dan barat(west) adalah 270 °.
Sekarang mari kita lihat pada notasi kuadran, alternatif untuk notasi azimuth.
Notasi Quadrant membagi muka kompas menjadi kuadran (pikirkan seperti memotong kue menjadi empat bagian yang sama). Ada timur laut(northeast), tenggara(southeast), barat daya(southwest), dan barat laut(northwest) kuadran. Sudut yang diukur timur atau barat dari utara dan timur atau barat selatan seperti gambar dibawah
Dalam notasi kuadran, Anda menentukan arah sebagai sejumlah derajat timur atau barat dari utara atau timur atau barat dari selatan (tergantung pada kuadran mana itu).
Timur laut(northeast) adalah 45 ° timur dari utara, tenggara(southeast) adalah 45 ° timur dari selatan, dan barat daya(southwest) adalah 45 ° barat selatan.
Beberapa arah dapat ditentukan dengan dua cara. Timur adalah 90 ° timur dari utara atau 90 ° sebelah timur dari selatan. Demikian pula untuk barat (itu 90 ° barat dari utara atau selatan). Utara adalah 0 ° timur dari utara atau 0 ° barat utara. Demikian pula untuk selatan (itu 0 ° timur atau barat dari selatan).
Cara yang benar untuk menulis notasi kuadran N atau S (untuk utara atau selatan), diikuti dengan 'angle', diikuti oleh E atau W (untuk timur atau barat). Oleh karena itu, N45 ° W adalah 45 ° barat dari utara atau barat laut.
Berikut adalah muka kompas diatur untuk notasi kuadran dan menunjukkan, ketepatan, N45 ° W.
Mengkonversi antara azimuth dan notasi kuadran adalah cukup sederhana asalkan Anda ingat bagaimana masing-masing ditentukan. Lihatlah gambar di bawah untuk membandingkan dua metode.
Saya pribadi lebih suka notasi azimut karena itu yang paling mudah untuk masuk ke dalam program komputer yang, misalnya, akan plot data dalam stereographic proyeksi (yang kita akan belajar tentang segera). Yang lain lebih memilih notasi kuadran, dan tidak ada yang salah dengan itu, tetapi hanya memastikan bahwa metode apapun yang Anda lakukan digunakan (dan itu mungkin akan tergantung pada jenis kompas yang Anda miliki) digunakan secara konsisten. Dengan kata lain, jangan terus beralih dari satu metode lain ketika pencatatan data atau Anda akan cepat menjadi bingung.
Deklinasi magnetik
Banyak orang tidak menyadari bahwa jarum kompas tidak biasanya menunjuk ke utara, tetapi pada beberapa sudut timur atau barat dari utara. Hal ini karena tiang geografis bumi (sumbu tentang yang berputar) tidak di tempat yang sama seperti kutub magnet nya (tempat di mana garis gaya magnetik muncul dari bumi). Arah ke kutub geografis bumi disebut True North dan arah ke kutub magnetik bumi dengan disebut utara magnetik.
Sebuah ekspedisi oleh Geological Survey of Canada pada tahun 1994 ditetapkan bahwa rata-rata posisi kutub magnet utara untuk tahun itu adalah 78,3 ° N, 104.0 ° W (dekat Ellef Ringnes Pulau di Arktik Kanada). Mereka juga menetapkan bahwa kutub magnet bergerak sekitar 15 km per tahun.
Jadi, jika Anda menggunakan sebuah kompas suatu tempat di permukaan bumi, Anda harus memperhitungkan perbedaan antara utara magnetik (dimana kompas menunjuk) dan utara yang benar (yang perlu Anda ketahui). Sudut antara True North dan utara magnetik disebut deklinasi magnetik dan perubahan dengan lokasi Anda dan, pada satu suatu lokasi, dengan waktu.
Bagaimana kita mengetahui berapa jadinya nilai deklinasi magnetis adalah?
Ada beberapa program komputer yang rapi menghitung deklinasi magnetik pada lintang dan bujur tertentu di permukaan bumi. Apa yang kebanyakan ahli geologi lakukan, bagaimanapun, hanya berkonsultasi dengan seorang pemetaan topografi untuk Area dibidangnya masing-masing, atau yang tersedia diterbitkan oleh USGS menerbitkan peta yang murah menunjukkan deklinasi magnetik di seluruh dunia.
Pada peta topografi yang khas, deklinasi magnetik ditunjukkan seperti berikut:
Bintang menunjukkan True North (ke arah atas hampir ke semua peta) dan MN menunjukkan arah ke kutub utara magnet dari pusat peta. Dalam kasus ini, kutub magnet utara adalah 15 ° barat dari True North.
Ada cara sederhana untuk mengoreksi deklinasi magnetik pada kebanyakan kompas. The Brunton kompas, yang akan dibahas segera, memiliki pin indeks di ujung utara dari cincin kompas (cincin di sekitar muka kompas dengan azimuths tercetak di atasnya). Bila kompas diatur untuk deklinasi 0 ° magnet, pin indeks sejajar dengan nol.
Ada setscrew kuningan di sisi kompas yang bergerak ke cincin kompas baik searah jarum jam atau berlawanan jarum jam. Satu-satunya trik dalam mengoreksi deklinasi magnetis adalah untuk mengingat cara untuk mengubah cincin kompas untuk timur dan barat deklinasi.
Untuk deklinasi magnetis 15 ° timur dari True North, Anda akan mengubah cincin kompas sehingga pin indeks lebih dari 15 ° (yaitu 15 ° ke sisi timur dari utara).
Untuk deklinasi 15 ° barat, Anda akan mengubah cincin kompas sehingga pin indeks lebih dari 345 ° (yaitu 15 ° ke sisi barat utara).
andai, misalnya, bahwa Anda telah menetapkan kompas untuk deklinasi 15 ° BT. Anda dapat memeriksa untuk melihat apakah pengaturan sudah benar dengan orientasi kompas sehingga ujung putih jarum pada 0 °. Putar kompas 15 ° BT dan jika ujung putih jarum menunjuk ke arah yang sama pada lengan penampakan untuk kompas Anda berada dalam bisnis.
The Brunton Compass
Ahli geologi menggunakan jenis khusus dari kompas, diciptakan pada tahun 1894 oleh insinyur pertambangan asal Kanada DW Brunton, yang biasa disebut, sebagai kompas Brunton. Kata "Brunton" sebenarnya adalah nama perusahaan,
Sejarah Singkat Kompas Brunton Klik Disini
Sumber : earthsci.org/compass