Add to ORKGABSTRACT The variation of soil color that developed on carbonate rocks which are generally white, very interesting to be studied. ...........................................................
A study was undertaken on the pedogenesis of a Podzol sequence of soils on the West Coast of Vancouv...
The accumulation of carbonate in soils is one of the most prominent soil forming processes in arid a...
Carbonate rock is a general term for the rock composed of carbonate minerals, which is mainly compos...
The variation of soil color that developed on carbonate rocks which are generally white, very intere...
The research is about soil variation profile in the outcrop around Gua Musang for identifying the min...
Western part of the East Jawa Southern Mountains, which is distributed from Parangtritis, Yogyakarta...
ABSTRAK The existence of pink and white limestones which are scattered sporadically at Klepu area of...
Soils of Universiti Pertanian Malaysia were surveyed and studied in order to determine their mineral...
Thirteen pedons representing the mountains, the upper footslopes, the lower footslopes, and the allu...
Measurements on modern soil color suggest well functional relationships between the soil formation p...
Revealing the pedogenesis of soil on carbonate rocks is a key step in determining the boundaries of ...
In the nature there is a possibility to mix carbonate and siliciclastic components. Jeffrey Mount ma...
The Ponjong pink limestone is located in the Gunungkidul Regency, approximately 60 km southeast of ...
Important pedogenic processes of soils formed on dolomitic limestones are affected by the degree of ...
Pedogenic carbonates are a good proxy of soil formation and functioning because the morphology of mi...
A study was undertaken on the pedogenesis of a Podzol sequence of soils on the West Coast of Vancouv...
The accumulation of carbonate in soils is one of the most prominent soil forming processes in arid a...
Carbonate rock is a general term for the rock composed of carbonate minerals, which is mainly compos...
The variation of soil color that developed on carbonate rocks which are generally white, very intere...
The research is about soil variation profile in the outcrop around Gua Musang for identifying the min...
Western part of the East Jawa Southern Mountains, which is distributed from Parangtritis, Yogyakarta...
ABSTRAK The existence of pink and white limestones which are scattered sporadically at Klepu area of...
Soils of Universiti Pertanian Malaysia were surveyed and studied in order to determine their mineral...
Thirteen pedons representing the mountains, the upper footslopes, the lower footslopes, and the allu...
Measurements on modern soil color suggest well functional relationships between the soil formation p...
Revealing the pedogenesis of soil on carbonate rocks is a key step in determining the boundaries of ...
In the nature there is a possibility to mix carbonate and siliciclastic components. Jeffrey Mount ma...
The Ponjong pink limestone is located in the Gunungkidul Regency, approximately 60 km southeast of ...
Important pedogenic processes of soils formed on dolomitic limestones are affected by the degree of ...
Pedogenic carbonates are a good proxy of soil formation and functioning because the morphology of mi...
A study was undertaken on the pedogenesis of a Podzol sequence of soils on the West Coast of Vancouv...
The accumulation of carbonate in soils is one of the most prominent soil forming processes in arid a...
Carbonate rock is a general term for the rock composed of carbonate minerals, which is mainly compos...