Salinity episodes and their reversal in the late pliocene of south-western Australia

IEECAS SKLLQG

Impact of Brunswick river mouth training walls on adjacent beaches, Brunswick heads, New South Wales, Australia

River training walls have been built at scores of locations along the NSW coast and their impacts on shoreline change are still not fully understood. In this study, the Brunswick River entrance and adjacent beaches are selected for examination of the impact of the construction of major training walls. Thirteen sets of aerial photographs taken between 1947 and 1994 are used in a CIS approach to accurately determine tire shoreline Position, beach contours and sand volumes, and their changes in both time and space, and then to assess the contribution of both tire structures and natural hydrodynamic conditions to large scale (years-decades and kilometres) beach changes. The impact of the training walls can be divided into four stages: natural conditions prior to their construction (pre 1959), major downdrift erosion and updrift accretion during and. following the construction of the walls in 1959 similar to 1962 and 1966. diminishing impact of the walls between 1966 and 1987, and finally no apparent impact between 1987 similar to 1994. The impact extends horizontally about 8 km updrift and 17 km downdrift, and temporally up to 25 years..

A comparative study of the resilience of coal logistics chains in Australia, South Africa and Canada

Au cours des dernières années l'industrie du charbon a connu un essor important. L'importance du charbon dans l'économie mondiale provient d'une demande mondiale soutenue et de niveaux de production en hausse constante. De ce fait, le nombre élevé d'importateurs et d'exportateurs est à l'origine d'un système d'échange complexe où la compétition est féroce. En effet, un nombre grandissant de pays importateurs se partagent les sources d'approvisionnement tandis qu'un nombre limité de pays exportateurs s'efforcent de répondre à la demande tout en essayant de s'accaparer le plus de parts du marché mondial. L'objectif de cette recherche s'inscrit dans ce contexte en démontrant les bénéfices associés aux chaînes logistiques résilientes pour tout acteur de l'industrie soucieux de devancer la compétition. Une analyse de la logistique de l'industrie du charbon permet entre autres de se pencher sur les questions suivantes: Comment les infrastructures influencent-elles la résilience d'une chaîne logistique? Quels risques est-ce que les catastrophes naturelles présentent pour une chaîne logistique? Comment la gouvernance influence-t-elle la résilience d'une chaîne logistique? Une chaîne logistique représente le trajet effectué par un bien ou produit au cours de son cycle de vie, du point d'origine au point de consommation. Ceci étant dit, le meilleur moyen de régler les problèmes inhérents aux chaînes logistiques est de maintenir de hauts niveaux de résilience. Cette recherche évaluera donc la résilience de chaînes logistiques du charbon des industries australienne, sud-africaine et canadienne. Pour ce faire, trois variables seront étudiées: les infrastructures, les catastrophes naturelles et la gouvernance. La comparaison des trois cas à l'étude se fera par un nombre défini d'indicateurs (12 au total) pour chacune des variables étudiées. Les résultats de cette recherche démontrent que la résilience des trois cas à l'étude se ressemble. Cependant, certaines chaînes logistiques détiennent des avantages comparatifs qui améliorent grandement leur résilience et leur compétitivité. Plusieurs sujets de recherche pourraient être utilisés pour compléter cette recherche. L'analyse comparative pourrait être appliquée à d'autres chaînes logistiques pour vérifier la viabilité des résultats. Une analyse semblable pourrait également être entreprise pour le secteur en aval de la chaîne logistique. Finalement, une méthodologie basée sur des interviews pourrait ajouter un regard différent sur les questions abordées.

The development of soil organic matter in restored biodiverse Jarrah forests of South-Western Australia as determined by ASE and GCMS

Background, aim and scope Soil organic matter (SOM) is known to increase with time as landscapes recover after a major disturbance; however, little is known about the evolution of the chemistry of SOM in reconstructed ecosystems. In this study, we assessed the development of SOM chemistry in a chronosequence (space for time substitution) of restored Jarrah forest sites in Western Australia. Materials and methods Replicated samples were taken at the surface of the mineral soil as well as deeper in the profile at sites of 1, 3, 6, 9, 12, and 17 years of age. A molecular approach was developed to distinguish and quantify numerous individual compounds in SOM. This used accelerated solvent extraction in conjunction with gas chromatography mass spectrometry. A novel multivariate statistical approach was used to assess changes in accelerated solvent extraction (ASE)-gas chromatography-mass spectrometry (GCMS) spectra. This enabled us to track SOM developmental trajectories with restoration time. Results Results showed total carbon concentrations approached that of native forests soils by 17 years of restoration. Using the relate protocol in PRIMER, we demonstrated an overall linear relationship with site age at both depths, indicating that changes in SOM chemistry were occurring. Conclusions The surface soils were seen to approach native molecular compositions while the deeper soil retained a more stable chemical signature, suggesting litter from the developing diverse plant community has altered SOM near the surface. Our new approach for assessing SOM development, combining ASE-GCMS with illuminating multivariate statistical analysis, holds great promise to more fully develop ASE for the characterisation of SOM.

Soil carbon and litter development along a reconstructed biodiverse forest chronosequence of South-Western Australia

Soil organic matter (SOM) increases with time as landscape is restored. Studying SOM development along restored forest chronosequences would be useful in clarifying some of the uncertainties in quantifying C turnover rates with respect to forest clearance and ensuing restoration. The development of soil organic matter in the mineral soils was studied at four depths in a 16-year-old restored jarrah forest chronosequence. The size-separated SOM fractionation along with δ13C isotopic shift was utilised to resolve the soil C temporal and spatial changes with developing vegetation. The restored forest chronosequence revealed several important insights into how soil C is developing with age. Litter accumulation outpaced the native forest levels in 12 years after restoration. The surface soils, in general, showed increase in total C with age, but this trend was not clearly observed at lower depths. C accumulation was observed with increasing restoration age in all three SOM size-fractions in the surface 0–2 cm depth. These biodiverse forests show a trend towards accumulating C in recalcitrant stable forms, but only in the surface 0–2 cm mineral soil. A significant reverse trend was observed for the moderately labile SOM fraction for lower depths with increasing restoration age. Correlating the soil δ13C with total C concentration revealed the re-establishment of the isotopically depleted labile to enriched refractory C continuum with soil depth for the older restored sites. This implied that from a pedogenic perspective, the restored soils are developing towards the original native soil carbon profile.