標(biāo)題: Titlebook: Ecology of a Glacial Flood Plain; J. V. Ward (former Head of Limnology),U. Uehlinger Book 2003 Springer Science+Business Media Dordrecht 2 [打印本頁] 作者: gingerly 時(shí)間: 2025-3-21 18:31
書目名稱Ecology of a Glacial Flood Plain影響因子(影響力)
書目名稱Ecology of a Glacial Flood Plain影響因子(影響力)學(xué)科排名
書目名稱Ecology of a Glacial Flood Plain網(wǎng)絡(luò)公開度
書目名稱Ecology of a Glacial Flood Plain網(wǎng)絡(luò)公開度學(xué)科排名
書目名稱Ecology of a Glacial Flood Plain被引頻次
書目名稱Ecology of a Glacial Flood Plain被引頻次學(xué)科排名
書目名稱Ecology of a Glacial Flood Plain年度引用
書目名稱Ecology of a Glacial Flood Plain年度引用學(xué)科排名
書目名稱Ecology of a Glacial Flood Plain讀者反饋
書目名稱Ecology of a Glacial Flood Plain讀者反饋學(xué)科排名
作者: 碌碌之人 時(shí)間: 2025-3-21 22:48
Groundwater-Surface Water Interactions,cal reservoirs of the catchment including ice, snow, and ground water. An alternative view is to look at streams as “part of the catchment’s downvalley and downgradient transport of water and solutes” (Bencala, 1993). From this perspective, water is transported through the catchment by overland, sur作者: Flatus 時(shí)間: 2025-3-22 03:54 作者: Thrombolysis 時(shí)間: 2025-3-22 06:59 作者: 軟膏 時(shí)間: 2025-3-22 12:27 作者: 闖入 時(shí)間: 2025-3-22 16:11
Terrestrial Floodplain Vegetation,ng the method of space-for-time substitution (Matthews, 1992). Investigations of the foreland vegetation in the Bernina massif included several studies (Burga, 1999; Flütsch, 1930; Lüdi, 1958; Richter, 1994; Rübel, 1912).作者: 闖入 時(shí)間: 2025-3-22 20:09 作者: 尖 時(shí)間: 2025-3-22 22:17 作者: FLORA 時(shí)間: 2025-3-23 04:17
Interstitial Fauna,(Füreder, 1999; Milner et al., 2000, 2001; Lods-Crozet et al. 2001). Ecological research conducted on 7 streams distributed across Europe, from the French Pyrenees to the arctic archipelago of Svalbard, provided insight into the factors affecting the composition and distribution of benthic invertebr作者: Conspiracy 時(shí)間: 2025-3-23 07:37
Organic Matter Dynamics,tochthonous primary production in the wetted channel and allochthonous inputs of organic detritus produced on the flood plains and uplands. The relative importance of autochthonous versus allochthonous production varies significantly along the river continuum as well as across geographical regions a作者: Harpoon 時(shí)間: 2025-3-23 09:41 作者: insert 時(shí)間: 2025-3-23 14:35
Nutrient Limitation,(see Chapter 12). Some side-slope tributaries do have substantial inputs of terrestrially derived organic matter, but these represent a small percentage of the total channel area in the flood plain (Zah & Uehlinger, 2001). Constraints on primary production vary by stream type and time of year. Chann作者: Allure 時(shí)間: 2025-3-23 18:46
Drift and Colonization Dynamics,t serves as an important colonization mechanism (Williams & Hynes, 1976; Müller, 1982; Mackay, 1992). Concomitant with the drift of invertebrates, stream currents also transport large amounts of particulate matter (e. g., Waringer, 1992), the temporal patterns of which reflect functional attributes 作者: 背叛者 時(shí)間: 2025-3-23 22:44 作者: Eosinophils 時(shí)間: 2025-3-24 03:29
Nutrient Dynamics, arctic areas (Tockner et al., 2002, and references therein). The fractionation of nutrients into dissolved and particulate forms, and into inorganic and organic components, is essential for a comprehensive understanding of nutrient dynamics.作者: onlooker 時(shí)間: 2025-3-24 08:08
Aquatic Hyphomycetes in Alpine Streams,heir prolific sporulation under water. The capacity of at least the non-tropical species to germinate, to grow and to reproduce at relatively low temperatures is another noteworthy feature (Ingold, 1975; Webster & Descals, 1981; B?rlocher, 1992a).作者: 矛盾 時(shí)間: 2025-3-24 13:42 作者: 誓言 時(shí)間: 2025-3-24 18:32
,Besondere Arten von Arbeitsverh?ltnissen,sensu Junk et al., 1989) is widely recognized as the major force structuring floodplain habitat conditions, even moderate increases in discharge (“flow pulses”) may result in dramatic expansion of inundated area and can be important in sustaining habitat heterogeneity in river flood plains (Tockner et al., 2000).作者: Eclampsia 時(shí)間: 2025-3-24 21:14
Karin Nipperdey,Reinhardt Seifertincoming stream flow and losses by radiation or latent heat exchange (Webb & Zhang, 1997). Heat budgets depend on the regional climate and local characteristics such as riparian vegetation, aspect, channel morphology, stream water-groundwater interactions and hydrology (Constanz, 1998; Gu et al., 1998; Hawkins et al., 1997; Ward, 1985).作者: flammable 時(shí)間: 2025-3-25 00:19 作者: 不容置疑 時(shí)間: 2025-3-25 06:07
Channel Typology,sensu Junk et al., 1989) is widely recognized as the major force structuring floodplain habitat conditions, even moderate increases in discharge (“flow pulses”) may result in dramatic expansion of inundated area and can be important in sustaining habitat heterogeneity in river flood plains (Tockner et al., 2000).作者: 恃強(qiáng)凌弱 時(shí)間: 2025-3-25 09:10
Thermal Heterogeneity,incoming stream flow and losses by radiation or latent heat exchange (Webb & Zhang, 1997). Heat budgets depend on the regional climate and local characteristics such as riparian vegetation, aspect, channel morphology, stream water-groundwater interactions and hydrology (Constanz, 1998; Gu et al., 1998; Hawkins et al., 1997; Ward, 1985).作者: 看法等 時(shí)間: 2025-3-25 15:21
Litter Decomposition,le in the litter dynamics of low elevation streams, tropical streams in particular (Flecker, 1996). In concert with various chemical changes, micro-organisms cause transformations in litter quality (e. g., increases in nitrogen and phosphorus concentrations) that influence decomposition dynamics (Webster & Benfield, 1986; Gessner et al., 1999).作者: 自制 時(shí)間: 2025-3-25 16:00
,Beendigung des Arbeitsverh?ltnisses,second order glacial stream that flows in a north-northeast direction before it joins the Bernina River near the village of Pontresina. The Roseg valley is part of the catchment of the Inn River, which is the major Alpine tributary of the upper Danube.作者: 遺留之物 時(shí)間: 2025-3-25 20:59 作者: embolus 時(shí)間: 2025-3-26 03:23
Val Roseg: A High Alpine Catchment,second order glacial stream that flows in a north-northeast direction before it joins the Bernina River near the village of Pontresina. The Roseg valley is part of the catchment of the Inn River, which is the major Alpine tributary of the upper Danube.作者: 過分 時(shí)間: 2025-3-26 04:43
Nutrient Limitation,now-cover and low nutrients limit primary production in most stream types in winter (Robinson et al., 2002). Nutrient dynamics also change longitudinally along the main channel because of the increase in tributary and groundwater inputs as one moves downstream (Malard et al., 1999; Tockner et al., 2002).作者: 捏造 時(shí)間: 2025-3-26 09:24 作者: irreparable 時(shí)間: 2025-3-26 14:40 作者: 集聚成團(tuán) 時(shí)間: 2025-3-26 17:46 作者: boisterous 時(shí)間: 2025-3-26 21:44 作者: 飛鏢 時(shí)間: 2025-3-27 01:58 作者: 放縱 時(shí)間: 2025-3-27 08:15
Terrestrial Floodplain Vegetation,ng the method of space-for-time substitution (Matthews, 1992). Investigations of the foreland vegetation in the Bernina massif included several studies (Burga, 1999; Flütsch, 1930; Lüdi, 1958; Richter, 1994; Rübel, 1912).作者: 放氣 時(shí)間: 2025-3-27 11:55
https://doi.org/10.1007/978-94-017-0181-5Ecology; Fauna; Flora; ecosystem; ecosystems; seasonal dynamics; temporal dynamics; vegetation作者: Projection 時(shí)間: 2025-3-27 15:45
978-90-481-6507-0Springer Science+Business Media Dordrecht 2003作者: botany 時(shí)間: 2025-3-27 17:55 作者: bypass 時(shí)間: 2025-3-28 01:44 作者: 新星 時(shí)間: 2025-3-28 02:54 作者: 青少年 時(shí)間: 2025-3-28 08:37
Beatrix Tr?ger,Nadja Ro?-KirschBased on their local water sources and temperature regimes, three principal types of streams, each with distinctive zoobenthic assemblages, occur in alpine environments (Ward, 1994):作者: 規(guī)范要多 時(shí)間: 2025-3-28 11:33 作者: 贊美者 時(shí)間: 2025-3-28 17:04 作者: 形容詞 時(shí)間: 2025-3-28 21:25 作者: 暫時(shí)中止 時(shí)間: 2025-3-28 23:00 作者: 盡忠 時(shí)間: 2025-3-29 04:46 作者: 機(jī)警 時(shí)間: 2025-3-29 10:51 作者: OATH 時(shí)間: 2025-3-29 15:19
Allgemeine Grundlagen des Arbeitsrechts,esses, and influence metabolic pathways in the riparian, parafluvial and hyporheic zones (e. g. Duff & Triska, 2000; Wetzel, 2001). Surprisingly few year-round studies, however, have quantified concentrations and fluxes of all major nutrient fractions; this is particularly true for remote alpine and作者: 天文臺(tái) 時(shí)間: 2025-3-29 18:33 作者: 一窩小鳥 時(shí)間: 2025-3-29 21:48 作者: Hiatal-Hernia 時(shí)間: 2025-3-30 00:47 作者: 嚙齒動(dòng)物 時(shí)間: 2025-3-30 05:34 作者: 裝勇敢地做 時(shí)間: 2025-3-30 09:30
,Aufnahme des Arbeitsverh?ltnisses,tochthonous primary production in the wetted channel and allochthonous inputs of organic detritus produced on the flood plains and uplands. The relative importance of autochthonous versus allochthonous production varies significantly along the river continuum as well as across geographical regions a作者: infatuation 時(shí)間: 2025-3-30 14:25
,Die Anstellung beim Betriebsübergang, information on stream functioning (nutrient cycling and energy flow). Analyses of decomposing litter also inform us about the distribution and abundance (structure) of stream biota such as fungi, bacteria, invertebrates, and fish. Leaf breakdown is caused by the joint action of physical factors cau作者: 不來 時(shí)間: 2025-3-30 17:18
,Pr?missen und Struktur der Expertise,(see Chapter 12). Some side-slope tributaries do have substantial inputs of terrestrially derived organic matter, but these represent a small percentage of the total channel area in the flood plain (Zah & Uehlinger, 2001). Constraints on primary production vary by stream type and time of year. Chann作者: debouch 時(shí)間: 2025-3-30 21:13 作者: Atheroma 時(shí)間: 2025-3-31 04:36
https://doi.org/10.1007/978-3-642-94306-5s Alps, encompassing landscape features and their history, physical and chemical characteristics of surface waters and ground waters, aquatic and terrestrial flora, benthic and hyporheic biota, and mechanistic studies of ecosystem function (Fig. 1). The results demonstrate the inherent dynamic compl作者: 無法取消 時(shí)間: 2025-3-31 05:29 作者: cathartic 時(shí)間: 2025-3-31 09:35
