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Статті в журналах з теми "Wombat State Forest (Vic )"

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Fest, Benedikt J., Nina Hinko-Najera, Tim Wardlaw, David W. T. Griffith, Stephen J. Livesley, and Stefan K. Arndt. "Soil methane oxidation in both dry and wet temperate eucalypt forests shows a near-identical relationship with soil air-filled porosity." Biogeosciences 14, no. 2 (January 27, 2017): 467–79. http://dx.doi.org/10.5194/bg-14-467-2017.

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Abstract. Well-drained, aerated soils are important sinks for atmospheric methane (CH4) via the process of CH4 oxidation by methane-oxidising bacteria (MOB). This terrestrial CH4 sink may contribute towards climate change mitigation, but the impact of changing soil moisture and temperature regimes on CH4 uptake is not well understood in all ecosystems. Soils in temperate forest ecosystems are the greatest terrestrial CH4 sink globally. Under predicted climate change scenarios, temperate eucalypt forests in south-eastern Australia are predicted to experience rapid and extreme changes in rainfall patterns, temperatures and wild fires. To investigate the influence of environmental drivers on seasonal and inter-annual variation of soil–atmosphere CH4 exchange, we measured soil–atmosphere CH4 exchange at high-temporal resolution (< 2 h) in a dry temperate eucalypt forest in Victoria (Wombat State Forest, precipitation 870 mm yr−1) and in a wet temperature eucalypt forest in Tasmania (Warra Long-Term Ecological Research site, 1700 mm yr−1). Both forest soil systems were continuous CH4 sinks of −1.79 kg CH4 ha−1 yr−1 in Victoria and −3.83 kg CH4 ha−1 yr−1 in Tasmania. Soil CH4 uptake showed substantial temporal variation and was strongly controlled by soil moisture at both forest sites. Soil CH4 uptake increased when soil moisture decreased and this relationship explained up to 90 % of the temporal variability. Furthermore, the relationship between soil moisture and soil CH4 flux was near-identical at both forest sites when soil moisture was expressed as soil air-filled porosity (AFP). Soil temperature only had a minor influence on soil CH4 uptake. Soil nitrogen concentrations were generally low and fluctuations in nitrogen availability did not influence soil CH4 uptake at either forest site. Our data suggest that soil MOB activity in the two forests was similar and that differences in soil CH4 exchange between the two forests were related to differences in soil moisture and thereby soil gas diffusivity. The differences between forest sites and the variation in soil CH4 exchange over time could be explained by soil AFP as an indicator of soil moisture status.
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Petheram, Lisa, and Digby Race. "What is a Good Forest? Ex-Forest worker perspectives from the Wombat State Forest (Victoria)." Rural Society 15, no. 1 (January 2005): 93–100. http://dx.doi.org/10.5172/rsj.351.15.1.93.

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Poynter, Mark. "Collaborative forest management in Victoria's Wombat State Forest — will it serve the interests of the wider community?" Australian Forestry 68, no. 3 (January 2005): 192–201. http://dx.doi.org/10.1080/00049158.2005.10674965.

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Silva, Andreza Gonçalves da, and Pedro B. Schwartsburd. "Ferns of Viçosa, Minas Gerais State, Brazil: Polypodiaceae (Polypodiales, Filicopsida, Tracheophyta)." Hoehnea 44, no. 2 (April 2017): 251–68. http://dx.doi.org/10.1590/2236-8906-95/2016.

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ABSTRACT As part of an ongoing project treating the ferns and lycophytes from the region of Viçosa, MG, Brazil, we here present the taxonomic treatment of Polypodiaceae. We performed field expeditions in remaining forest patches and disturbed sites from 2012 to 2016. We also revised the Polypodiaceae collection of VIC herbarium. In the region of Viçosa, 19 species of Polypodiaceae occur: Campyloneurum centrobrasilianum, C. decurrens, C. lapathifolium, C. phyllitidis, Cochlidium punctatum, Microgramma crispata, M. percussa, M. squamulosa, M. vacciniifolia, Niphidium crassifolium, Pecluma filicula, P. plumula, P. truncorum, Phlebodium areolatum, P. decumanum, Pleopeltis astrolepis, P. minima, Serpocaulon fraxinifolium, and S. menisciifolium. Among them, six are endemic to the Atlantic Forest. During our search in VIC, we found an isotype of Campyloneurum centrobrasilianum. We present keys, descriptions, illustrations, examined materials, and comments of all taxa.
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Duclos, Loris. "Response to ‘Collaborative forest management in Victoria's Wombat State Forest — will it serve the interests of the wider community?’." Australian Forestry 69, no. 1 (January 2006): 72. http://dx.doi.org/10.1080/00049158.2006.10674991.

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Ward, S. J. "The efficacy of nestboxes versus spotlighting for detecting feathertail gliders." Wildlife Research 27, no. 1 (2000): 75. http://dx.doi.org/10.1071/wr99018.

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A series of spotlight transects were carried out over a two-year period within a 7-ha area of the Wombat State Forest, Victoria, which contained nestboxes used by feathertail gliders, Acrobates pygmaeus. Spotlighting was carried out on foot through open forest, not along tracks, and only one feathertail glider was detected in 13.8 h of spotlighting. The nestboxes were checked on days following spotlighting surveys and 72 captures of feathertail gliders were made over the same two- year period. Spotlighting can provide important information on the biology of feathertail gliders when used in long-term scientific studies by experienced spotlighters. However, it is an unsatisfactory technique for broad surveys of feathertail gliders, and nestboxes provide a better technique but require a longer time-frame and additional cost.
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Lunney, D., and M. Oconnell. "Habitat Selection by the Swamp Wallaby, Wallabia-Bicolor, the Red-Necked Wallaby, Macropus-Rufogriseus, and the Common Wombat, Vombatus-Ursinus, in Logged, Burnt Forest Near Bega, New-South-Wales." Wildlife Research 15, no. 6 (1988): 695. http://dx.doi.org/10.1071/wr9880695.

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This study examined the habitat selected by the swamp wallaby, Wallabia bicolor, the red-necked wallaby, Macropus rufogriseus, and the common wombat, Vombatus ursinus. The habitats were unlogged forest and three age classes of logged forest at 16 weeks and 72 weeks after a fire in November 1980 in Mumbulla State Forest on the south coast ofNew South Wales. Habitat selection was determined from decay-corrected dung counts. The dung count for each species varied with the topography and age class of the forest, demonstrating that logging and fire had a marked effect on the habitat selected. The ridges logged during the woodchip-sawlog operation in 1979 and 1980 had little dung, indicating low use as feeding areas. Since these habitats were the most exposed, the conclusion drawn was that they were rarely used by the herbivores. However, ridges logged 10-15 years earlier supported all species because they provided both food and refuge shelter. Recommendations for management of forests subject to logging and fire include the retention of unlogged gully forest and spreading operations through both space and time to minimise population fluctuations.
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Tomkins, IB, JD Kellas, KG Tolhurst, and DA Oswin. "Effects of fire intensity on soil chemistry in a eucalypt forest." Soil Research 29, no. 1 (1991): 25. http://dx.doi.org/10.1071/sr9910025.

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Soil samples taken in the Wombat State Forest in Victoria, at depths of 0-2, 2-5, and 5-10 cm before and after burning fuel loads of 0 (unburnt control), 15, 50, 150, and 300 t ha-1 were analysed for pH, exchangeable cations and cation exchange capacity, available and total P, organic carbon and soil moisture, over a 2-year, 2000 mm rainfall period. Short term responses (up to 6 months) occurred in levels of exchangeable NH4+, K+, and Mg2+, and long term changes (2 years or longer) over the period of the study were observed for pH, available and total P and exchangeable ca2+ at the 0-2 cm soil depth for the burnt treatments. Following burning (and 108 mm of rain), changes in soil chemical parameters were strongly correlated with fuel load and the quantity of fuel burnt. Changes through the 0-10 cm profile for the various chemical parameters are described, together with seasonal variations. For similar yellow podzolic soils, measurement of soil pH may be a useful criterion for monitoring soil chemical changes following slash and fuel reduction burning, provided that accurate estimates of fuel loads, composition and amount burnt can be established.
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PERKINS, PHILIP D. "A revision of the Australian species of the water beetle genus Hydraena Kugelann (Coleoptera: Hydraenidae)." Zootaxa 1489, no. 1 (May 31, 2007): 1–207. http://dx.doi.org/10.11646/zootaxa.1489.1.1.

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The Australian species of the water beetle genus Hydraena Kugelann, 1794, are revised, based on the study of 7,654 specimens. The 29 previously named species are redescribed, and 56 new species are described. The species are placed in 24 species groups. High resolution digital images of all primary types are presented (online version in color), and geographic distributions are mapped. Male genitalia, representative female terminal abdominal segments and representative spermathecae are illustrated. Australian Hydraena are typically found in sandy/gravelly stream margins, often in association with streamside litter; some species are primarily pond dwelling, a few species are humicolous, and one species may be subterranean. The areas of endemicity and species richness coincide quite closely with the Bassian, Torresian, and Timorian biogeographic subregions. Eleven species are shared between the Bassian and Torresian subregions, and twelve are shared between the Torresian and Timorian subregions. Only one species, H. impercepta Zwick, is known to be found in both Australia and Papua New Guinea. One Australian species, H. ambiflagellata, is also known from New Zealand. New species of Hydraena are: H. affirmata (Queensland, Palmerston National Park, Learmouth Creek), H. ambiosina (Queensland, 7 km NE of Tolga), H. antaria (New South Wales, Bruxner Flora Reserve), H. appetita (New South Wales, 14 km W Delagate), H. arcta (Western Australia, Synnot Creek), H. ascensa (Queensland, Rocky Creek, Kennedy Hwy.), H. athertonica (Queensland, Davies Creek), H. australula (Western Australia, Synnot Creek), H. bidefensa (New South Wales, Bruxner Flora Reserve), H. biimpressa (Queensland, 19.5 km ESE Mareeba), H. capacis (New South Wales, Unumgar State Forest, near Grevillia), H. capetribensis (Queensland, Cape Tribulation area), H. converga (Northern Territory, Roderick Creek, Gregory National Park), H. cubista (Western Australia, Mining Camp, Mitchell Plateau), H. cultrata (New South Wales, Bruxner Flora Reserve), H. cunninghamensis (Queensland, Main Range National Park, Cunningham's Gap, Gap Creek), H. darwini (Northern Territory, Darwin), H. deliquesca (Queensland, 5 km E Wallaman Falls), H. disparamera (Queensland, Cape Hillsborough), H. dorrigoensis (New South Wales, Dorrigo National Park, Rosewood Creek, upstream from Coachwood Falls), H. ferethula (Northern Territory, Cooper Creek, 19 km E by S of Mt. Borradaile), H. finniganensis (Queensland, Gap Creek, 5 km ESE Mt. Finnigan), H. forticollis (Western Australia, 4 km W of King Cascade), H. fundaequalis (Victoria, Simpson Creek, 12 km SW Orbost), H. fundata (Queensland, Hann Tableland, 13 km WNW Mareeba), H. hypipamee (Queensland, Mt. Hypipamee National Park, 14 km SW Malanda), H. inancala (Queensland, Girraween National Park, Bald Rock Creek at "Under-ground Creek"), H. innuda (Western Australia, Mitchell Plateau, 16 mi. N Amax Camp), H. intraangulata (Queensland, Leo Creek Mine, McIlwrath Range, E of Coen), H. invicta (New South Wales, Sydney), H. kakadu (Northern Territory, Kakadu National Park, Gubara), H. larsoni (Queensland, Windsor Tablelands), H. latisoror (Queensland, Lamington National Park, stream at head of Moran's Falls), H. luminicollis (Queensland, Lamington National Park, stream at head of Moran's Falls), H. metzeni (Queensland, 15 km NE Mareeba), H. millerorum (Victoria, Traralgon Creek, 0.2 km N 'Hogg Bridge', 5.0 km NNW Balook), H. miniretia (Queensland, Mt. Hypipamee National Park, 14 km SW Malanda), H. mitchellensis (Western Australia, 4 km SbyW Mining Camp, Mitchell Plateau), H. monteithi (Queensland, Thornton Peak, 11 km NE Daintree), H. parciplumea (Northern Territory, McArthur River, 80 km SW of Borroloola), H. porchi (Victoria, Kangaroo Creek on Springhill Rd., 5.8 km E Glenlyon), H. pugillista (Queensland, 7 km N Mt. Spurgeon), H. queenslandica (Queensland, Laceys Creek, 10 km SE El Arish), H. reticuloides (Queensland, 3 km ENE of Mt. Tozer), H. reticulositis (Western Australia, Mining Camp, Mitchell Plateau), H. revelovela (Northern Territory, Kakadu National Park, GungurulLookout), H. spinissima (Queensland, Main Range National Park, Cunningham's Gap, Gap Creek), H. storeyi (Queensland, Cow Bay, N of Daintree River), H. tenuisella (Queensland, 3 km W of Batavia Downs), H. tenuisoror (Australian Capital Territory, Wombat Creek, 6 km NE of Piccadilly Circus), H. textila (Queensland, Laceys Creek, 10 km SE El Arish), H. tridisca (Queensland, Mt. Hemmant), H. triloba (Queensland, Mulgrave River, Goldsborough Road Crossing), H. wattsi (Northern Territory, Holmes Jungle, 11 km NE by E of Darwin), H. weiri (Western Australia, 14 km SbyE Kalumburu Mission), H. zwicki (Queensland, Clacherty Road, via Julatten).
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Guerova, G., and N. Jones. "2003 megafires in Australia: impact on tropospheric ozone and aerosols." Atmospheric Chemistry and Physics Discussions 9, no. 1 (January 29, 2009): 3007–40. http://dx.doi.org/10.5194/acpd-9-3007-2009.

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Abstract. 2003 was a record year for wildfires worldwide. Severe forest fires killed four people, displaced 20 500 others and burnt 260 000 ha in South-East Australia in January 2003. The uncontrolled fires ignited in early January 2003 as a result of a prolonged El Niño drought in South-East Australia. Severe weather conditions resulted in a fast spread of the fires and poor air quality in a region where 70% of the population of Australia lives. We use state-of-art global chemistry and transport model GEOS-Chem in conjunction with ground- and space-based observations to study the ozone (O3) and aerosol enhancement due to fires. Firstly, the monthly mean surface O3 and Aerosol Optical Depth (AOD) in January 2003 are compared to January 2004 and, secondly, from sensitivity model simulations, four episodes are isolated and an attempt is made to quantify the contribution of the fires to air quality in south and South-East Australia. In January 2003 the observed monthly mean afternoon surface O3 in Victoria (VIC) and South Australia (SA) reached 27.5 ppb, which is 6.5 ppb (i.e. 30%) higher than in 2004. The simulated O3 is 29.5 ppb, which is 10 ppb higher than in 2004. While the model tends to overestimate the observed peak O3, it exhibits very good skill in reproducing the O3 temporal variability in January 2003 with a correlation of 0.83. In VIC, the air quality 4-h ozone (O3) standard exceedences are reported on 17, 24 and 25 January. On 12, 17, 24–25 and 29 January 2003, the observed O3 peaks above 40 ppb and the simulated fire contribution is higher than 10 ppb. During these 4 episodes, the range of observed O3 enhancement due to fires is 20–35 ppb, which is a factor of 3 to 5 higher than the monthly mean. The simulated fire O3 enhancement is in the range 15–50 ppb with a factor of 1.5 to 5 higher than the monthly mean. During two episodes, a well-formed surface wind channel stretches across the Tasman Sea facilitating the long range transport to New Zealand contributing to a 10% increase of surface O3. During the four episodes in January 2003, the observed AOD was up to a factor of five higher that the monthly mean AOD. The simulated and observed AODs agree on the spatial structure. Despite the model tendency to underestimate the AOD, it proves a useful tool in reconstructing the mostly patchy observations.
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Книги з теми "Wombat State Forest (Vic )"

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Caricias Del Mar: Unidos Por el Mar. Harlequin Enterprises, Limited, 2010.

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Частини книг з теми "Wombat State Forest (Vic )"

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"involve either the rejection of sexual love or its abuse. love chastely but want sexual satisfaction now, for Although Guyon is the servant of the ‘heauenly example Timias at v 48. The lowest stair is occupied Mayd’ (II i 28.7), he never sees the one and only by those who pervert love, either through jealousy spies on the other before binding her and ravaging in loving a woman as an object (as Malbecco at ix 5) her bower. From the opening episode of Book III, it or in using force to satisfy their desire (as Busirane becomes evident that Guyon’s binding of Acrasia has at xi 11). Book III is aptly named ‘the book of sex’ initiated an action that requires the rest of the poem by M. Evans 1970:152, for Spenser’s anatomy of to resolve, namely, how to release women from male love extends outward to the natural order and the tyranny, and therefore release men from their desire cosmos, and to the political order in which the ‘Most to tyrannize women. Chastity is fulfilled when its famous fruites of matrimoniall bowre’ (iii 3.7) are patron, Britomart, frees Amoret from Busirane’s the progeny of English kings. tyranny; friendship is fulfilled when Florimell’s chaste To fashion the virtues of the first two books, love for Marinell leads to her being freed from Spenser uses the motif of the single quest: a knight is Proteus’s tyranny; and Artegall is able to fulfil the guided to his goal, one by Una and the other by the virtue of justice when his lover, Britomart, frees him Palmer, and on his way engages in chivalric action from Radigund’s tyranny to which he has submitted. usually in the open field. To fashion chastity, he uses By destroying Acrasia’s sterile bower of perpetual the romance device of entrelacement, the interweav-summer, Guyon frees Verdant, whose name invokes ing of separate love stories into a pattern of relation-spring with its cycle of regeneration. The temperate ships. (As the stories of the four squires in Books III body, seen in the Castle of Alma, ‘had not yet felt and IV form an interlaced narrative, see Dasenbrock Cupides wanton rage’ (II ix 18.2), but with the cycle 1991:52–69.) The variety of love’s pageants requires of the seasons, love enters the world: ‘all liuing multiple quests, and the action shifts to the forest, wights, soone as they see | The spring breake forth the seashore, and the sea (see ‘Places, allegorical’ and out of his lusty bowres, | They all doe learne to play ‘Sea’ in the SEnc). Thus Britomart, guided by ‘blind the Paramours’ (IV x 45). Once the temperate body loue’ (IV v 29.5), wanders not knowing where to has felt ‘Cupides wanton rage’ in Book III, knights find her lover. As she is a virgin, her love for Artegall lie wounded or helpless and their ladies are either in is treated in the Belphœbe–Timias story; as she seeks flight or imprisoned – all except Britomart, who, to fulfil her love in marriage, her relationship to though as sorely wounded by love as any, is armed Artegall is treated in the Scudamour–Amoret story; with chastity, which controls her desire as she follows and as her marriage has the apocalyptic import ‘the guydaunce of her blinded guest’ (III iv 6.8), prophesied by Merlin at III iii 22–23, its significance that is, her love for Artegall. in relation to nature is treated in the Marinell– Book III presents an anatomy of love, its motto Florimell story. Like Florimell, Britomart loves a being ‘Wonder it is to see, in diuerse mindes, | How knight faithfully; but, like Marinell (see iv 26.6), diuersly loue doth his pageaunts play, | And shewes Artegall scorns love (see IV vi 28.9), neither know-his powre in variable kindes’ (v 1). While there is ing that he is loved. Yet Florimell knows whom she only one Cupid, his pageants vary, then, according to loves while Britomart does not, having seen only his diverse human states. If only because the poem is image. In contrast to both, Amoret loves faithfully, dedicated to the Virgin Queen, virginity is accorded and is loved faithfully in return; and in contrast to all, ‘the highest stayre | Of th’honorable stage of Belphœbe does not know that she is loved by Timias womanhead’ (v 54.7–8), being represented in Book and does not love him. (To complete this scheme: at III by Belphœbe. She was ‘vpbrought in perfect III vii 54, Columbell knows that she is loved by the Maydenhed’ by Diana, while her twin (yet later Squire of Dames but withholds love for him.) The born) sister, Amoret, was ‘vpbrought in goodly pattern formed by these stories fashions the virtue of womanhed’ (vi 28.4, 7) by Venus. Accordingly, chastity of which Britomart is the patron. Amoret occupies the central stair of chaste love, for Since interlaced narratives take the place of the lin-she loves Scudamour faithfully and is rescued by ear quest, Spenser structures Book III by balancing Britomart, the virgin who loves Artegall faithfully. the opening and concluding cantos against the mid-Since both are chaste, their goal is marriage in which dle canto. Canto vi is the book’s centre as it treats." In Spenser: The Faerie Queene, 33. Routledge, 2014. http://dx.doi.org/10.4324/9781315834696-31.

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