Nutrients for plant growth are often limited in soil systems and additions are required in the form of fertiliser. Potassium is an essential macro-nutrient for plants and demands for K are expected to increase in the future. Glaucony is an abundant marine mineral which may provide an alternative K-rich fertiliser resource. The South Island of New Zealand contains deposits of glaucony-rich rocks which were deposited in the Early- to Mid-Cenozoic during periods of low sedimentation to the seafloor. Here, the geochemistry of glaucony from the Waitaki Basin (Otago), the Waipara Greensand (North Canterbury) and the Stoney Creek Limestone (Karamea) was examined using spatially resolved geochemical analysis and dissolution experiments. Grain-by-gr...
Growth of world population and consequent growth of food demand are drivers of expansion and intensi...
This study presents a review on palaeogeographic implications and temporal variations of glaucony co...
Glauconite is usually found as a replacement of bioclasts and faecal pellets through neoformation an...
Glauconite occurs as the major constituent of late Cretaceous and Tertiary greensand deposits formed...
An integrated study involving sedimentology, mineral chemistry and spectroscopy highlights a distinc...
A detailed mineral chemical investigation of glauconite within the condensed section deposits of the...
Potassium is one of the important nutrients for healthy growth and development of plants. This artic...
minerals in a soil profile developed on a gtauconite sand indicate that destabilization f glauconite...
Chatham Rise is a broad, elongated submarine platform that extends 1100 km out into the Southwest Pa...
This study examines factors favouring optimal release of potassium from a glauconitic rock by modera...
The availability of potassium to pasture plants in New Zealand is dependent upon the mineralogy of t...
Glauconite must be assessed as mica-rich mica-smectite R3 interstratified mineral, with the pure end...
Petrographic examination was carried out on glauconites of Cretaceous or Lower Tertiary age from 142...
This paper explores suitability of glauconitic rocks in the Upper Cretaceous Bakchar deposit in West...
International audienceThis work examines the possibility of a rapid formation of glauconite in a rel...
Growth of world population and consequent growth of food demand are drivers of expansion and intensi...
This study presents a review on palaeogeographic implications and temporal variations of glaucony co...
Glauconite is usually found as a replacement of bioclasts and faecal pellets through neoformation an...
Glauconite occurs as the major constituent of late Cretaceous and Tertiary greensand deposits formed...
An integrated study involving sedimentology, mineral chemistry and spectroscopy highlights a distinc...
A detailed mineral chemical investigation of glauconite within the condensed section deposits of the...
Potassium is one of the important nutrients for healthy growth and development of plants. This artic...
minerals in a soil profile developed on a gtauconite sand indicate that destabilization f glauconite...
Chatham Rise is a broad, elongated submarine platform that extends 1100 km out into the Southwest Pa...
This study examines factors favouring optimal release of potassium from a glauconitic rock by modera...
The availability of potassium to pasture plants in New Zealand is dependent upon the mineralogy of t...
Glauconite must be assessed as mica-rich mica-smectite R3 interstratified mineral, with the pure end...
Petrographic examination was carried out on glauconites of Cretaceous or Lower Tertiary age from 142...
This paper explores suitability of glauconitic rocks in the Upper Cretaceous Bakchar deposit in West...
International audienceThis work examines the possibility of a rapid formation of glauconite in a rel...
Growth of world population and consequent growth of food demand are drivers of expansion and intensi...
This study presents a review on palaeogeographic implications and temporal variations of glaucony co...
Glauconite is usually found as a replacement of bioclasts and faecal pellets through neoformation an...