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Volcanic particles in agriculture and gardening
Uppsala universitet, Teknisk-naturvetenskapliga vetenskapsområdet, Geovetenskapliga sektionen, Institutionen för geovetenskaper, Mineralogi, petrologi och tektonik.
Uppsala universitet, Teknisk-naturvetenskapliga vetenskapsområdet, Geovetenskapliga sektionen, Institutionen för geovetenskaper, Mineralogi, petrologi och tektonik.
Uppsala universitet, Teknisk-naturvetenskapliga vetenskapsområdet, Geovetenskapliga sektionen, Institutionen för geovetenskaper, Paleobiologi.
Visa övriga samt affilieringar
2017 (Engelska)Ingår i: Geology Today, ISSN 0266-6979, E-ISSN 1365-2451, Vol. 33, nr 4, s. 148-154Artikel i tidskrift (Refereegranskat) Published
Abstract [en]

Volcanic pyroclasts of small size, such as lapilli and small pumice stones, are widely used in agriculture, gardening, and for pot plants as natural inorganic mulch. The technique of using pyroclasts to enhance topsoil stems from the eighteenth century, and specifically from the ad 1730–1736 eruption on Lanzarote. Critical observations on plant development during and after the eruption showed that the vegetation died when buried under a thick layer of lapilli, but grew vigorously when covered thinly. While the agriculture of Lanzarote was restricted to cereals before the eruption, it diversified to many kinds of fruit and vegetables afterwards, including the production of the famous Malvasía wines in the Canaries. The population of Lanzarote doubled in the years after the eruption, from about 5000 in 1730 to near 10 000 in 1768, predominantly as a result of the higher agricultural productivity. This outcome led to widespread use of lapilli and pumice fragments throughout the islands and eventually the rest of the globe. Lapilli and pumice provide vesicle space for moisture to be retained longer within the planting soil, which can create an environment for micro-bacteria to thrive in. Through this route, nutrients from volcanic matter are transported into the surrounding soil where they become available to plant life. The detailed processes that operate within the pyroclasts are less well understood, such as the breakdown of nutrients from the rock matrix and transport into the soil by biological action. Further studies promise significant potential to optimize future agricultural efforts, particularly in otherwise arid areas of the globe.

Ort, förlag, år, upplaga, sidor
2017. Vol. 33, nr 4, s. 148-154
Nationell ämneskategori
Multidisciplinär geovetenskap
Identifikatorer
URN: urn:nbn:se:uu:diva-383079DOI: 10.1111/gto.12193OAI: oai:DiVA.org:uu-383079DiVA, id: diva2:1314526
Tillgänglig från: 2019-05-09 Skapad: 2019-05-09 Senast uppdaterad: 2019-09-03Bibliografiskt granskad
Ingår i avhandling
1. Trans-crustal magma storage in contrasting tectonic settings
Öppna denna publikation i ny flik eller fönster >>Trans-crustal magma storage in contrasting tectonic settings
2019 (Engelska)Doktorsavhandling, sammanläggning (Övrigt vetenskapligt)
Abstract [en]

Magmatic plumbing systems comprise magma chambers, sheet intrusions, and conduits which link the Earth’s deep interior with the Earth’s surface. As such, they are the structural framework of magma transport and storage that is governed by complex physical and chemical processes in magma reservoirs and through the interaction of magma bodies with surrounding crustal rocks over timescales from hours to millions of years. These geological processes, in turn, play a vital role in controlling eruptive behaviour and the magnitude of associated volcanic eruptions that impact the environment as well as human society. Our understanding of the nature and location of magmatic processes and plumbing system architecture remains, however, fragmentary. This lack of knowledge can partly be attributed to limits regarding the spatial resolution of geophysical methods and partly to geochemical uncertainties and errors in associated models. Ongoing advances in analytical techniques increase spatial, temporal, and chemical resolution, hence enabling us to gather more detailed knowledge on the structure and dynamics of magmatic systems, especially for individual volcanoes, but also in respect to the long-term evolution of magmatic provinces and ultimately the Earth as a whole. This process-oriented thesis examines fossil and active magmatic plumbing systems in Iceland, Indonesia, Cameroon, and the Canary Islands by applying a combination of traditional and state-of-the-art petrological and geochemical methods, mineral(-melt) thermobarometric modelling, and isotopic analytical techniques. The results add valuable insights to the growing body of evidence for multi-tiered plumbing systems in a number of volcano-tectonic settings and underline the importance of shallow-level magma storage and its influence on magma evolution and hazardous volcanic eruptions.

Ort, förlag, år, upplaga, sidor
Uppsala: Acta Universitatis Upsaliensis, 2019. s. 45
Serie
Digital Comprehensive Summaries of Uppsala Dissertations from the Faculty of Science and Technology, ISSN 1651-6214 ; 1818
Nyckelord
magma plumbing systems, thermobarometry, oxygen isotope analysis, shallow arc storage systems
Nationell ämneskategori
Geokemi
Identifikatorer
urn:nbn:se:uu:diva-383081 (URN)978-91-513-0673-5 (ISBN)
Disputation
2019-09-06, Hambergsalen, Geocentrum, Villavägen 16, Uppsala, 09:00 (Engelska)
Opponent
Handledare
Tillgänglig från: 2019-06-10 Skapad: 2019-05-09 Senast uppdaterad: 2019-08-23

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Förlagets fulltexthttps://onlinelibrary.wiley.com/doi/abs/10.1111/gto.12193

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Troll, Valentin R.Streng, MichaelBarker, AbigailDeegan, FrancesGeiger, Harri
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