Soil CO2 flux baseline in an urban monogenetic volcanic field: the Auckland Volcanic Field, New Zealand

2013 ◽  
Vol 75 (11) ◽  
Author(s):  
Agnès Mazot ◽  
Elaine R. Smid ◽  
Luitgard Schwendenmann ◽  
Hugo Delgado-Granados ◽  
Jan Lindsay
Keyword(s):  
New Zealand ◽  
Co2 Flux ◽  
Volcanic Field ◽  
Soil Co2 ◽  
Auckland Volcanic Field ◽  
Soil Co2 Flux ◽  
Monogenetic Volcanic Field

USING PYROCLASTIC TEXTURES TO UNDERSTAND DYNAMIC ERUPTION PROCESSES IN THE AUCKLAND VOLCANIC FIELD, NEW ZEALAND

2018 ◽  
Author(s):  
Megan M. Ferguson ◽  
◽  
Michael C. Rowe ◽  
Manuela Tost ◽  
Karoly Nemeth
Keyword(s):  
New Zealand ◽  
Volcanic Field ◽  
Auckland Volcanic Field

scholarly journals K‐Ar ages, paleomagnetism, and geochemistry of the South Auckland volcanic field, North Island, New Zealand

1994 ◽  
Vol 37 (2) ◽  
pp. 143-153 ◽  
Author(s):  
R. M. Briggs ◽  
T. Okada ◽  
T. Itaya ◽  
H. Shibuya ◽  
I. E. M. Smith
Keyword(s):  
New Zealand ◽  
Volcanic Field ◽  
The South ◽  
Auckland Volcanic Field

scholarly journals Composite development and stratigraphy of the Onepoto maar lake sediment sequence (Auckland Volcanic Field, New Zealand)

2021 ◽  
Vol 29 ◽  
pp. 19-37
Author(s):  
Benjamin Läuchli ◽  
Paul Christian Augustinus ◽  
Leonie Peti ◽  
Jenni Louise Hopkins
Keyword(s):  
New Zealand ◽  
Lake Sediment ◽  
Volcanic Field ◽  
Tuff Ring ◽  
Auckland Volcanic Field ◽  
14C Dating ◽  
Quaternary Climate ◽  
Laminated Sediment ◽  
Continuous Record ◽  
Maar Lake

Abstract. The accurate and precise reconstruction of Quaternary climate as well as the events that punctuate it is an important driver of the study of lake sediment archives. However, until recently lake sediment-based palaeoclimate reconstructions have largely concentrated on Northern Hemisphere lake sequences due to a scarcity of continuous and high-resolution lake sediment sequences from the Southern Hemisphere, especially from the southern mid-latitudes. In this context, the deep maar lakes of the Auckland Volcanic Field of northern New Zealand are significant as several contain continuous and well-laminated sediment sequences. Onepoto Basin potentially contains the longest temporal lake sediment record from the Auckland Volcanic Field (AVF), spanning from Marine Isotope Stage 6e (MIS 6e) to the early Holocene when lacustrine sedimentation was terminated by marine breach of the south-western crater tuff ring associated with post-glacial sea-level rise. The Onepoto record consists of two new, overlapping cores spanning ca. 73 m combined with archive material in a complete composite stratigraphy. Tephrochronology and 14C dating provide the fundamental chronological framework for the core, with magnetic relative palaeo-intensity variability downcore, and meteoric 10Be influx into the palaeolake to refine the chronology. The µ-XRF (micro X-ray fluorescence) downcore variability for the entirety of the lake sediment sequence has been established with measurement of a range of proxies for climate currently underway. This work will produce the first continuous record of the last 200 kyr of palaeoclimate from northern New Zealand to date.

scholarly journals Spatial and Temporal Variability of Soil CO2 Flux in Sugarcane Green Harvest Systems

2016 ◽  
Vol 40 (0) ◽  
Author(s):  
Rose Luiza Moraes Tavares ◽  
Zigomar Menezes de Souza ◽  
Newton La Scala Jr ◽  
Guilherme Adalberto Ferreira Castioni ◽  
Gustavo Soares de Souza ◽  
...  
Keyword(s):  
Temporal Variability ◽  
Co2 Flux ◽  
Spatial And Temporal Variability ◽  
Soil Co2 ◽  
Soil Co2 Flux

scholarly journals Comparative soil CO2 flux measurements and geostatistical estimation methods on Masaya volcano, Nicaragua

2005 ◽  
Vol 68 (1) ◽  
pp. 76-90 ◽  
Author(s):  
Jennifer L. Lewicki ◽  
Deborah Bergfeld ◽  
Carlo Cardellini ◽  
Giovanni Chiodini ◽  
Domenico Granieri ◽  
...  
Keyword(s):  
Co2 Flux ◽  
Estimation Methods ◽  
Soil Co2 ◽  
Soil Co2 Flux ◽  
Masaya Volcano ◽  
Geostatistical Estimation ◽  
Flux Measurements

Biocrust contribution to soil CO2 flux in desert shrubland ecosystem of northwest Mexico

2021 ◽  
pp. 1-17
Author(s):  
Fernando Ayala-Niño ◽  
Yolanda Maya-Delgado ◽  
Enrique Troyo-Diéguez ◽  
Pedro P. Garcillán
Keyword(s):  
Co2 Flux ◽  
Soil Co2 ◽  
Soil Co2 Flux ◽  
Northwest Mexico ◽  
Desert Shrubland

scholarly journals VARIABILIDADE ESPACIAL DO FLUXO DE CO2 DO SOLO EM POVOAMENTO DE EUCALIPTO

FLORESTA ◽  
2011 ◽  
Vol 41 (2) ◽  
Author(s):  
Alexandre Fonseca D’Andréa ◽  
Marx Leandro Naves Silva ◽  
Diego Antonio França de Freitas ◽  
Nilton Curi ◽  
Carlos Alberto Silva
Keyword(s):  
Organic Matter ◽  
Environmental Factors ◽  
Organic Carbon ◽  
Spatial Variability ◽  
Linear Correlation ◽  
Microbial Biomass Carbon ◽  
Co2 Flux ◽  
Water Evaporation ◽  
Soil Co2 ◽  
Soil Co2 Flux

A matéria orgânica do solo armazena a maior parte do carbono contido nos sistemas terrestres do planeta, sendo a maioria encontrada nos solos com floresta. O objetivo deste trabalho foi quantificar o fluxo de CO2 do solo e a sua variabilidade espacial em povoamento de Eucalyptus sp. Foram avaliados o fluxo de CO2 do solo, fatores ambientais (evaporação de água, temperatura e umidade do solo), atributos relacionados à fertilidade (pH, soma de bases e alumínio trocável), estrutura (densidade do solo e porosidade total) e matéria orgânica do solo (carbono orgânico total e carbono da biomassa microbiana). Análises de correlação linear simples indicaram que parte da variabilidade espacial do fluxo de CO2 do solo pode ser explicada pelo efeito conjunto do teor de carbono orgânico do solo, da biomassa da serapilheira e da presença de árvores no terreno, indicativas da participação de fatores bióticos no processo. No entanto, o fluxo de CO2 do solo é um fenômeno de natureza complexa, não sendo possível identificar um único atributo do solo ou do ambiente que, isoladamente, explique sua variação no espaço.Palavras-chave: Matéria orgânica; fatores ambientais; fertilidade; carbono; respiração do solo.AbstractSoil CO2 flux spatial variability on eucalyptus manmade forest.  The organic matter on soil retains most of carbon contained in the planet terrestrial systems, specially in forest soils. The aim of this work was to quantify soil CO2 flux and its spatial variability on Eucalyptus sp. manmade forest. In order to that, soil CO2 flux, environmental factors (water evaporation, soil temperature and moisture), fertility attributes (pH, bases sum and exchangeable aluminum), structure (bulk density and total porosity), and soil organic matter (total organic carbon and microbial biomass carbon) were evaluated. Simple linear correlation analyses indicated that part of the spatial variability of soil CO2 flux can be explained by the associated effect of soil organic carbon amount, litter biomass and presence of trees, indicatives of participation of biotic factors in the process. However, the soil CO2 flux is a complex phenomenon, been impossible to identify a single soil or environmental attribute, which, individually, could explain its spatial variability. Keywords: Organic matter; environmental factors; fertility; carbon; linear correlation. 

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