Coners, Heinz

[["dc.bibliographiccitation.firstpage","754"],["dc.bibliographiccitation.journal","Science of The Total Environment"],["dc.bibliographiccitation.lastpage","771"],["dc.bibliographiccitation.volume","648"],["dc.contributor.author","Miehe, Georg"],["dc.contributor.author","Schleuss, Per-Marten"],["dc.contributor.author","Seeber, Elke"],["dc.contributor.author","Babel, Wolfgang"],["dc.contributor.author","Biermann, Tobias"],["dc.contributor.author","Braendle, Martin"],["dc.contributor.author","Chen, Fahu"],["dc.contributor.author","Coners, Heinz"],["dc.contributor.author","Foken, Thomas"],["dc.contributor.author","Gerken, Tobias"],["dc.contributor.author","Graf, Hans-F."],["dc.contributor.author","Guggenberger, Georg"],["dc.contributor.author","Hafner, Silke"],["dc.contributor.author","Holzapfel, Maika"],["dc.contributor.author","Ingrisch, Johannes"],["dc.contributor.author","Kuzyakov, Yakov"],["dc.contributor.author","Lai, Zhongping"],["dc.contributor.author","Lehnert, Lukas"],["dc.contributor.author","Leuschner, Christoph"],["dc.contributor.author","Li, Xiaogang"],["dc.contributor.author","Liu, Jianquan"],["dc.contributor.author","Liu, Shibin"],["dc.contributor.author","Ma, Yaoming"],["dc.contributor.author","Miehe, Sabine"],["dc.contributor.author","Mosbrugger, Volker"],["dc.contributor.author","Noltie, Henry J."],["dc.contributor.author","Schmidt, Joachim"],["dc.contributor.author","Spielvogel, Sandra"],["dc.contributor.author","Unteregelsbacher, Sebastian"],["dc.contributor.author","Wang, Yun"],["dc.contributor.author","Willinghöfer, Sandra"],["dc.contributor.author","Xu, Xingliang"],["dc.contributor.author","Yang, Yongping"],["dc.contributor.author","Zhang, Shuren"],["dc.contributor.author","Opgenoorth, Lars"],["dc.contributor.author","Wesche, Karsten"],["dc.date.accessioned","2020-12-10T15:21:13Z"],["dc.date.available","2020-12-10T15:21:13Z"],["dc.date.issued","2019"],["dc.identifier.doi","10.1016/j.scitotenv.2018.08.164"],["dc.identifier.issn","0048-9697"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/72951"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-354"],["dc.title","The Kobresia pygmaea ecosystem of the Tibetan highlands – Origin, functioning and degradation of the world's largest pastoral alpine ecosystem"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","329"],["dc.bibliographiccitation.issue","3"],["dc.bibliographiccitation.journal","Environmental and Experimental Botany"],["dc.bibliographiccitation.lastpage","336"],["dc.bibliographiccitation.volume","71"],["dc.contributor.author","Graefe, Sophie"],["dc.contributor.author","Leuschner, Christoph"],["dc.contributor.author","Coners, Heinz"],["dc.contributor.author","Hertel, Dietrich"],["dc.date.accessioned","2018-11-07T08:54:55Z"],["dc.date.available","2018-11-07T08:54:55Z"],["dc.date.issued","2011"],["dc.description.abstract","Lowered temperatures may reduce the root water uptake of tropical trees at high elevations through several mechanisms; however, field studies to test their relevance are lacking. We measured sap flux density (J) in small-diameter tree roots across a 2000-m elevation transect in a tropical mountain forest for quantifying the effects of temperature (T(a)), VPD and soil moisture (theta) on root water flow and uptake at different elevations. Recently developed miniature heat balance-sap flow gauges were applied to roots of about 10 mm in diameter in mountain forest stands at 1050, 1890 and 3060m a.s.l. in the Ecuadorian Andes and the measured flow was related to anatomical properties of the root xylem. Between 1050 and 3060 m, mean J decreased to about a third. VPD was the most influential environmental factor controlling J at 1050 and 1890 m, while T(a) was the key determinant at 3060 in. Large vessels were absent in the root xylem of high-elevation trees which resulted in a 10-fold decrease of theoretical hydraulic conductivity (k(h)(theor)) between 1050 and 3060 in. We conclude that both physical limitations (reduced VPD, increased viscosity of water) and biological constraints (large decrease of k(h)(theor)) result in a significantly reduced J and root water uptake of the trees in high-elevation tropical forests. (C) 2011 Elsevier B.V. All rights reserved."],["dc.description.sponsorship","German Science Foundation (DFG) through Research Group [402, B6]"],["dc.identifier.doi","10.1016/j.envexpbot.2011.01.001"],["dc.identifier.isi","000290013500001"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/22785"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Pergamon-elsevier Science Ltd"],["dc.relation.issn","0098-8472"],["dc.title","Root functioning in tropical high-elevation forests: Environmental vs. biological control of root water absorption"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.journal","Plant Ecology"],["dc.contributor.author","Ibe, Karin"],["dc.contributor.author","Walmsley, David"],["dc.contributor.author","Fichtner, Andreas"],["dc.contributor.author","Coners, Heinz"],["dc.contributor.author","Leuschner, Christoph"],["dc.contributor.author","Härdtle, Werner"],["dc.date.accessioned","2021-12-01T09:23:29Z"],["dc.date.available","2021-12-01T09:23:29Z"],["dc.date.issued","2021"],["dc.identifier.doi","10.1007/s11258-021-01195-5"],["dc.identifier.pii","1195"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/94663"],["dc.language.iso","en"],["dc.notes.intern","DOI-Import GROB-478"],["dc.relation.eissn","1573-5052"],["dc.relation.iserratumof","/handle/2/80966"],["dc.relation.issn","1385-0237"],["dc.title","Correction to: Provenance- and life-history stage-specific responses of the dwarf shrub Calluna vulgaris to elevated vapour pressure deficit"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.subtype","erratum_ja"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","1359"],["dc.bibliographiccitation.issue","12"],["dc.bibliographiccitation.journal","Tree Physiology"],["dc.bibliographiccitation.lastpage","1367"],["dc.bibliographiccitation.volume","24"],["dc.contributor.author","Leuschner, C."],["dc.contributor.author","Coners, H."],["dc.contributor.author","Icke, R."],["dc.date.accessioned","2018-11-07T10:43:43Z"],["dc.date.available","2018-11-07T10:43:43Z"],["dc.date.issued","2004"],["dc.description.abstract","The spatial heterogeneity of water uptake by fine roots under field conditions was analyzed in situ with miniature sap flow gauges in a mature beech-oak-spruce mixed stand. Sap flow rate (J), sap flow density (J(d)), and root surface-area-specific flow rate (uptake rate, J(s)) were measured for eight to 10 small-diameter roots (3-4 mm) per species in the organic layer (superficial roots) and in the mineral soil (30-80 cm, deep roots) during four months in summer 1999. We calculated J(s) by relating J to the surface area of the section of the fine root system distal to the position of the gauge on the root. When measured synchronously, roots of the three species did not differ significantly in mean J(s), although oak roots tended to have lower rates. However, J(d) decreased in the sequence spruce > beech > oak in most measurement periods. Microscopic investigation revealed differences in fine root anatomy that may partly explain the species differences in J(d) and J(s). Oak fine roots had a thicker periderm than beech and spruce roots of similar diameter and spruce roots had fewer fine branch rootlets than the other species. Synchronously recorded J(d) and J(s) of nearby roots of the same tree species showed large differences in flow with coefficients of variation from 25 to 150% that could not be explained by patchy distribution of soil water. We hypothesize that the main cause of the large spatial heterogeneity in root water uptake is associated with differences between individual roots in morphology and ultrastructure of the root cortex that affect root radial and root-soil interface conductivities. The high intraspecific variation in J(s) may mask species differences in root water uptake. Superficial roots of all species typically had about five times higher J(d) than deep roots of the same species. However, J(s) values were similar for superficial and deep roots in beech and spruce because small diameter roots of both species were more branched in the organic layer than in mineral soil. In oak, deep roots had lower J(s) (maximum of 100 g m(-2) day(-1)) than superficial roots (about 1000 g m(-2) day(-1)). We conclude that temperate tree species in mixed stands have different water uptake capacities. Water flow in the rhizosphere of forests appears to be a highly heterogeneous process that is influenced by both tree species and differences in uptake rates of individual roots within a species."],["dc.identifier.isi","000225591200005"],["dc.identifier.pmid","15465698"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/47118"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Heron Publishing"],["dc.relation.issn","0829-318X"],["dc.title","In situ measurement of water absorption by fine roots of three temperate trees: species differences and differential activity of superficial and deep roots"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","86"],["dc.bibliographiccitation.issue","1"],["dc.bibliographiccitation.journal","Oikos"],["dc.bibliographiccitation.lastpage","97"],["dc.bibliographiccitation.volume","125"],["dc.contributor.author","Lübbe, Torben"],["dc.contributor.author","Schuldt, Bernhard"],["dc.contributor.author","Coners, Heinz"],["dc.contributor.author","Leuschner, Christoph"],["dc.date.accessioned","2017-11-28T10:03:30Z"],["dc.date.available","2017-11-28T10:03:30Z"],["dc.date.issued","2016"],["dc.description.abstract","Studies examining the influence of biodiversity on ecosystem functioning have rarely considered water turnover, the quantitatively most important biogeochemical flux in ecosystems and a process with high sensitivity to climate warming. With a tree sapling experiment consisting of three diversity levels (1, 3, 5 species), 11 different species combinations and two soil moisture levels (moist and dry), we examined the influence of tree species diversity and species identity on stand transpiration (T) under ample and restricted water supply. We further asked whether growth in mixture leads to adaptive responses in the hydraulic system and water loss regulation in plants with heterospecific neighbors compared to plants in monoculture. In moist soil, T was on average ∼11% higher in the mixtures than in the monocultures (significant net diversity effect), which can mostly be attributed to a selection effect. Overyielding in T was highest in mixtures when Tilia cordata and/or Fraxinus excelsior were present. Both species developed larger leaf areas (LA) and sapwood areas (SA) in monocultures than the other species and furthermore increased LA and SA from the monocultures to the mixtures. Thus, inherent species differences in LA and hydraulics, but also neighbor effects on these traits determined T to a large extend. In dry soil, the diversity effect on T was not larger but slightly smaller, which is not in agreement with other published studies. We conclude that differences between pure and mixed sapling assemblages in stand water consumption and drought response are mainly caused by species identity effects, while species diversity seems to be less influential."],["dc.identifier.doi","10.1111/oik.02367"],["dc.identifier.fs","620662"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/10603"],["dc.language.iso","en"],["dc.notes.status","final"],["dc.relation.eissn","1600-0706"],["dc.relation.issn","0030-1299"],["dc.title","Species diversity and identity effects on the water consumption of tree sapling assemblages under ample and limited water supply"],["dc.type","journal_article"],["dc.type.internalPublication","unknown"],["dc.type.peerReviewed","unknown"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","151"],["dc.bibliographiccitation.journal","Agricultural and Forest Meteorology"],["dc.bibliographiccitation.lastpage","161"],["dc.bibliographiccitation.volume","244-245"],["dc.contributor.author","Fuchs, Sebastian"],["dc.contributor.author","Leuschner, Christoph"],["dc.contributor.author","Link, Roman"],["dc.contributor.author","Coners, Heinz"],["dc.contributor.author","Schuldt, Bernhard"],["dc.date.accessioned","2018-02-26T10:42:20Z"],["dc.date.available","2018-02-26T10:42:20Z"],["dc.date.issued","2017"],["dc.description.abstract","Sap flow probes are routinely used in forest and horticulture hydrology for estimating tree water use. This requires unbiased measurements when upscaling from tree to stand level, but accuracy and comparability of different thermometric methods have been questioned. Three sap flow measuring techniques were compared against gravimetric flow measurement in cut stem segments: ‘Granier-type’ thermal dissipation probes (TDP; three different sensor types), the heat field deformation method (HFD), and the heat ratio method (HRM). For the empirical methods (TDP and HFD), new calibration parameters were estimated using a nonlinear hierarchical modelling approach. 66 stem segments from five temperate, diffuse-porous tree species (9–16 cm stem diameter, 100 cm stem length) were exposed to a wide range of flux densities by applying subatmospheric pressure (−50 to −650 hPa) analogous to natural flow conditions in the field. All TDP probes underestimated flux density by 23–45% when calculated with Granier's original calibration parameters, with the deviation increasing with flux rate. The accuracy was significantly improved by estimating new calibration parameters, especially for probes differing from Granier's original sensor design. Species-specific parameters further improved accuracy, although the species differences might partially be explained by variation in the observed ranges of sap flux. The HFD sensor overestimated gravimetric flow by ∼11%; empirical calibration did not improve its accuracy compared to the manufacturer's equation. At low to medium flow rates, the HRM system achieved higher accuracy than the other probes (0.8% underestimation), while performing poorly at high flux rates under our measurement settings (energy input of 25 J). Both for TDP and HFD sensors, we observed a surprisingly large variability in calibration parameters between different stems of the same species. We conclude that (i) TDP and HFD sensors require species-specific calibration to measure sap flux with high accuracy, (ii) the original Granier equation cannot be used for TDP probes with deviating design, and (iii), at low to medium flow rates, the highest accuracy can be achieved with HRM sensors. Our results help to increase the accuracy of tree sap flow measurements with thermal dissipation probes, and to assess various levels of errors related to the different thermometric methods. This is important when synthesizing forest transpiration data on regional and global scales."],["dc.identifier.doi","10.1016/j.agrformet.2017.04.003"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/12609"],["dc.language.iso","en"],["dc.notes.status","final"],["dc.title","Calibration and comparison of thermal dissipation, heat ratio and heat field deformation sap flow probes for diffuse-porous trees"],["dc.type","journal_article"],["dc.type.internalPublication","unknown"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","1219"],["dc.bibliographiccitation.issue","12"],["dc.bibliographiccitation.journal","Plant Ecology"],["dc.bibliographiccitation.lastpage","1232"],["dc.bibliographiccitation.volume","221"],["dc.contributor.author","Ibe, Karin"],["dc.contributor.author","Walmsley, David"],["dc.contributor.author","Fichtner, Andreas"],["dc.contributor.author","Coners, Heinz"],["dc.contributor.author","Leuschner, Christoph"],["dc.contributor.author","Härdtle, Werner"],["dc.date.accessioned","2021-04-14T08:23:34Z"],["dc.date.available","2021-04-14T08:23:34Z"],["dc.date.issued","2020"],["dc.identifier.doi","10.1007/s11258-020-01076-3"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/80966"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-399"],["dc.relation.eissn","1573-5052"],["dc.relation.haserratum","/handle/2/94663"],["dc.relation.issn","1385-0237"],["dc.title","Provenance- and life-history stage-specific responses of the dwarf shrub Calluna vulgaris to elevated vapour pressure deficit"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","763"],["dc.bibliographiccitation.issue","8"],["dc.bibliographiccitation.journal","Annals of Forest Science"],["dc.bibliographiccitation.lastpage","772"],["dc.bibliographiccitation.volume","60"],["dc.contributor.author","Leuschner, C."],["dc.contributor.author","Coners, H."],["dc.contributor.author","Icke, R."],["dc.contributor.author","Hartmann, K."],["dc.contributor.author","Effinger, N. D."],["dc.contributor.author","Schreiber, Laura Maria"],["dc.date.accessioned","2018-11-07T10:34:12Z"],["dc.date.available","2018-11-07T10:34:12Z"],["dc.date.issued","2003"],["dc.description.abstract","The water absorption by terminal branch roots of mature oak, beech and spruce trees was measured in situ with miniature sap flow gauges for 11 consecutive days and related to the suberin and lignin content of the fine root periderm. All fine roots contained a well-developed periderm, whereas no primary white roots were present. Mean root water uptake decreased in the sequence beech - spruce - oak. Oak roots contained twice as much suberin and a thicker periderm than beech, and had smaller mean water uptake rates (201 vs. 508 g m(-2) root surface d(-1)). However, spruce with 2 to 7 times smaller suberin contents had lower uptake rates (346 g m(2) d(-1)) than beech with more suberin. We conclude that the relationship between periderm chemistry and water absorption is only weak in the three species. Other factors such as hydraulic resistances in the soil-root interface, or the size of water potential gradients may be more influential in regulating root water uptake."],["dc.identifier.doi","10.1051/forest:2003071"],["dc.identifier.isi","000221039000003"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/44806"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","E D P Sciences"],["dc.relation.issn","1286-4560"],["dc.title","Chemical composition of the periderm in relation to in situ water absorption rates of oak, beech and spruce fine roots"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","395"],["dc.bibliographiccitation.issue","4"],["dc.bibliographiccitation.journal","Basic and Applied Ecology"],["dc.bibliographiccitation.lastpage","405"],["dc.bibliographiccitation.volume","6"],["dc.contributor.author","Coners, H."],["dc.contributor.author","Leuschner, C."],["dc.date.accessioned","2018-11-07T08:34:52Z"],["dc.date.available","2018-11-07T08:34:52Z"],["dc.date.issued","2005"],["dc.description.abstract","Miniature heat balance-sap flow gauges were used to measure water flows in small-diameter roots (3-4 mm) in the undisturbed soil of a mature beech-oak-spruce mixed stand. By relating sap flow to the surface area of all branch fine roots distal to the gauge, we were able to calculate real time water uptake rates per root surface area (J(S)) for individual fine root systems of 0.5-1.0m in length. Study aims were (i) to quantify root water uptake of mature trees under field conditions with respect to average rates, and diurnal and seasonal changes of J(S), and (ii) to investigate the relationship between uptake and soil moisture theta, atmospheric saturation deficit D, and radiation 1. On most days, water uptake followed the diurnal course of D with a midday peak and low night flow. Neighbouring roots of the same species differed up to 10-fold in their daily totals of J(S) ( < 100-2000 g m(-2) d(-1)) indicating a large spatial heterogeneity in uptake. Beech, oak and spruce roots revealed different seasonal patterns of water uptake although they were extracting water from the same soil volume. Multiple regression analyses on the influence of D, I and theta on root water uptake showed that D was the single most influential environmental factor in beech and oak (variable selection in 77% and 79% of the investigated roots), whereas D was less important in spruce roots (50% variable selection). A comparison of root water uptake with synchronous leaf transpiration (porometer data) indicated that average water fluxes per surface area in the beech and oak trees were about 2.5 and 5.5 times smaller on the uptake side (roots) than on the loss side (leaves) given that all branch roots < 2 mm were equally participating in uptake. Beech fine roots showed maximal uptake rates on mid-summer days in the range of 48-205 g m-2 h(-1) (i.e. 0.7-3.2 mmol m(-2) s(-1)), oak of 12-160 g m(-2) h(-1) (0.2-2.5 mmol m(-2) s(-1)). transpiration rates ranged from 3 to 5 and from 5 to 6 mmol m(-2) s(-1) for sun canopy leaves of beech and oak, respectively. We conclude that instantaneous rates of root water uptake in beech, oak and spruce trees are above all controlled by atmospheric factors. The effects of different root conductivities, soil moisture, and soil hydraulic properties become increasingly important if time spans longer than a week are considered. (c) 2005 Gesellschaft fur Okologie. Published by Elsevier GmbH. All rights reserved."],["dc.identifier.doi","10.1016/j.baae.2004.12.003"],["dc.identifier.isi","000231934600008"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/17924"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Urban & Fischer Verlag"],["dc.relation.issn","1439-1791"],["dc.title","In situ measurement of fine root water absorption in three temperate tree species - Temporal variability and control by soil and atmospheric factors"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","696"],["dc.bibliographiccitation.issue","5"],["dc.bibliographiccitation.journal","Functional Ecology"],["dc.bibliographiccitation.lastpage","703"],["dc.bibliographiccitation.volume","16"],["dc.contributor.author","Coners, H."],["dc.contributor.author","Leuschner, C."],["dc.date.accessioned","2018-11-07T09:59:26Z"],["dc.date.available","2018-11-07T09:59:26Z"],["dc.date.issued","2002"],["dc.description.abstract","1. Root water uptake is a key process in the circulation of water in forest ecosystems. Until recently, water absorption by tree fine roots could not be measured in situ in undisturbed soil. 2. We present a new technique that allows continuous recording of the water absorption of fine root endings in mature stands without altering soil structure, hydrology or mycorrhizal infection. 3. The approach combines miniature sap-flow gauges mounted on small-diameter tree roots (3-4 mm) with a complete extraction and visual surface analysis of the adjacent absorbing fine root endings. This technique yields continuous data on water absorption per fine root surface area, and allows analysis of the spatial heterogeneity of root water uptake in the rhizosphere of forests. 4. We present the results of laboratory and field calibration experiments with Fagus sylvatica L. roots (3-4 mm), which show a good agreement between gauge flow data and synchronous gravimetric flow measurements for flows between 2 and >50 g h(-1) . Gauge readings were unreliable during low flows (<2 g h(-1) ) at night. In these periods, which cover approximate to10% of daily flow, we used an empirically derived linear relationship between root temperature difference and flow. 5. Measurements on F. sylvatica root endings during 10 summer days showed daily water absorption maxima ranging between 0.20 (rainy days) and 0.58 mmol m(-2) root surface area s(-1) (bright or overcast days). The corresponding daily maxima of leaf transpiration rate were approximate to10 times higher (2-4 mmol m(-2) leaf area s(-1) ). 6. The combination of miniature sap-flow gauges and determination of fine root surface area provides a promising tool for analysing water absorption by tree root systems in situ ."],["dc.identifier.doi","10.1046/j.1365-2435.2002.00665.x"],["dc.identifier.isi","000178119300018"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/37586"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Blackwell Publishing Ltd"],["dc.relation.issn","0269-8463"],["dc.title","In situ water absorption by tree fine roots measured in real time using miniature sap-flow gauges"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]