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The first modern KBBI dictionary was published during the 5th Indonesian Language Congress on 28 October 1988. The first edition contains approximately 62,000 entries. The dictionary was compiled by a team led by the Head of the Language Center, Anton M. Moeliono , with chief editors Sri Sukesi Adiwimarta and Adi Sunaryo.
Tanah is the Malay/Indonesian word for soil, land or island. It can be found in topography. Tanah Abang – a market district in Jakarta, Indonesia; Tanah Datar – a regency in West Sumatra, Indonesia; Tanah Lot – a temple in Bali, Indonesia; Tanah Merah (disambiguation)
In Indonesia, however, there is a clear distinction between "Malay language" (bahasa Melayu) and "Indonesian" (bahasa Indonesia). Indonesian is the national language which serves as the unifying language of Indonesia; despite being a standardized form of Malay, it is not referred to with the term "Malay" in common parlance. [ 18 ]
Karena semua dibiayai menggunakan dana negara jutaan rupiah, baginda maharaja bijaksana, sang mahaguru sastra bahasa Kawi, mahasiswa-mahasiswi perguruan swasta, duta-duta negeri mitra dan suami/istrinya, Menteri Kebudayaan dan Pariwisata, karyawan-karyawati perusahaan ketenaga kerjaan, bupati budiman, beserta anggota lembaga nirlaba kewanitaan ...
The main processes of soil formation of oxisols are weathering, humification and pedoturbation due to animals. These processes produce the characteristic soil profile.They are defined as soils containing at all depths no more than ten percent weatherable minerals, and low cation exchange capacity.
A pH of 9.5 has 10 −9.5 moles hydronium ions per litre of solution (and also 10 −2.5 moles per litre OH −). A pH of 3.5 has one million times more hydronium ions per litre than a solution with pH of 9.5 (9.5 − 3.5 = 6 or 10 6) and is more acidic. [115] The effect of pH on a soil is to remove from the soil or to make available certain ions.
Vertisols have a high content of expansive clay minerals, many of them belonging to the montmorillonites that form deep cracks in drier seasons or years. In a phenomenon known as argillipedoturbation, alternate shrinking and swelling causes self-ploughing, where the soil material consistently mixes itself, causing some vertisols to have an extremely deep A horizon and no B horizon.
In soil classification, an Umbrisol is a soil with a dark topsoil and in which organic matter has accumulated within the mineral surface soil—in most cases with low base saturation—to the extent that it significantly affects the behaviour and utilization of the soil.