Corre, Marife D.

[["dc.bibliographiccitation.firstpage","123"],["dc.bibliographiccitation.issue","3"],["dc.bibliographiccitation.journal","SOIL"],["dc.bibliographiccitation.lastpage","137"],["dc.bibliographiccitation.volume","3"],["dc.contributor.author","de Blécourt, Marleen"],["dc.contributor.author","Corre, Marife D."],["dc.contributor.author","Paudel, Ekananda"],["dc.contributor.author","Harrison, Rhett D."],["dc.contributor.author","Brumme, Rainer"],["dc.contributor.author","Veldkamp, Edzo"],["dc.date.accessioned","2020-12-10T18:47:55Z"],["dc.date.available","2020-12-10T18:47:55Z"],["dc.date.issued","2017"],["dc.identifier.doi","10.5194/soil-3-123-2017"],["dc.identifier.eissn","2199-398X"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/78945"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-354"],["dc.title","Spatial variability in soil organic carbon in a tropical montane landscape: associations between soil organic carbon and land use, soil properties, vegetation, and topography vary across plot to landscape scales"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","42"],["dc.bibliographiccitation.journal","Geoderma"],["dc.bibliographiccitation.lastpage","50"],["dc.bibliographiccitation.volume","284"],["dc.contributor.author","Allen, Kara"],["dc.contributor.author","Corre, Marife D."],["dc.contributor.author","Kurniawan, Syahrul"],["dc.contributor.author","Utami, Sri Rahayu"],["dc.contributor.author","Veldkamp, Edzo"],["dc.date.accessioned","2017-09-07T11:43:32Z"],["dc.date.available","2017-09-07T11:43:32Z"],["dc.date.issued","2016"],["dc.description.abstract","Forest conversion to agriculture can decrease soil nutrient stocks overtime. However, inherent spatial variability in soil biochemical properties in converted landscapes could be high, and may supersede effects of land-use change on soil nutrient changes. Our aims were to assess changes in soil nutrient stocks with land-use change, and to quantify the proportions of spatial variability and land-use change effects on the overall variance of soil nutrient stocks. This study was conducted in Jambi Province, Sumatra, Indonesia in two distinct landscapes defined by the dominant soil texture and type: loam and clay Acrisol soils. In each landscape, four land-use types were examined: lowland forest and rubber interspersed in naturally regenerating forest (referred here as “jungle rubber”) as reference land uses and smallholder plantations of rubber and oil palm. In the 0–0.5 m soil depth of the reference land uses, the clay Acrisol had higher total N (660.1 ± 63.8–1074.2 ± 158.8 g N m− 2; P ≤ 0.05), exchangeable Ca (24.1 ± 5.7–80.6 ± 22.8 g Ca m− 2; P ≤ 0.06), Mg (4.3 ± 0.6–39.2 ± 16.3 g Mg m− 2; P ≤ 0.02), K (11.7 ± 0.7–34.7 ± 12.1 g K m− 2; P ≤ 0.06), extractable P (1.1 ± 0.1–2.6 ± 0.1 g P m− 2; P ≤ 0.001) and effective cation exchange capacity (ECEC; 11.4 ± 3.1–40.6 ± 11.0 cmolc kg− 1; P = 0.02), illustrating that clay content influenced soil fertility in these highly weathered soils. Compared to the reference land uses, the oil palm plantations had higher soil pH (4.2 ± 0.0–4.6 ± 0.1; P ≤ 0.04), base saturation (8.9 ± 1.6–6.5 ± 1.3%; P ≤ 0.07) and extractable P (0.8 ± 0.1–6.1 ± 3.2 g P m− 2; P ≤ 0.01) in the top 0.5 m depth, which was probably due to the legacy effect of biomass burning and fertilization. We were unable to detect significant effects of land-use change on other soil biochemical characteristics (i.e., ECEC, stocks of exchangeable bases, soil organic carbon (SOC), total N). Based on variance components analysis, a large proportion of the variance of these parameters was accounted by the variation among replicate plots (26–91%) rather than by land-use types (only 0–6%). Power analysis showed that the optimum number of replicate plots to detect land-use change effects on these parameters ranged from 5 to 7. Our results suggest that spatial variability must be represented in the experimental design in order to detect land-use change effects on soil nutrient changes through stratifying the area of inference (i.e., landscape or region) based on known drivers of soil fertility and determining the optimal number of experimental units."],["dc.identifier.doi","10.1016/j.geoderma.2016.08.010"],["dc.identifier.gro","3150168"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/6903"],["dc.language.iso","en"],["dc.notes.status","public"],["dc.relation","SFB 990: Ökologische und sozioökonomische Funktionen tropischer Tieflandregenwald-Transformationssysteme (Sumatra, Indonesien)"],["dc.relation","SFB 990 | A | A05: Optimierung des Nährstoffmanagements in Ölpalmplantagen und Hochrechnung plot-basierter Treibhausgasflüsse auf die Landschaftsebene transformierter Regenwälder"],["dc.relation.issn","0016-7061"],["dc.subject","Soil nutrient stocks; Lowland forest; Rubber; Oil palm; Land-use change"],["dc.subject.gro","sfb990_journalarticles"],["dc.title","Spatial variability surpasses land-use change effects on soil biochemical properties of converted lowland landscapes in Sumatra, Indonesia"],["dc.type","journal_article"],["dc.type.internalPublication","unknown"],["dc.type.peerReviewed","no"],["dc.type.subtype","original_ja"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.artnumber","117522"],["dc.bibliographiccitation.journal","Forest Ecology and Management"],["dc.bibliographiccitation.volume","451"],["dc.contributor.author","Tchiofo Lontsi, Rodine"],["dc.contributor.author","Corre, Marife D."],["dc.contributor.author","van Straaten, Oliver"],["dc.contributor.author","Veldkamp, Edzo"],["dc.date.accessioned","2019-12-13T16:52:30Z"],["dc.date.available","2019-12-13T16:52:30Z"],["dc.date.issued","2019"],["dc.description.abstract","Although disturbances associated with selective logging can cause pronounced changes in soil characteristics and nutrient stocks, such information is very limited for highly weathered soils in Africa. We assessed the effects of reduced impact logging (RIL, with a 30-year rotation management plan) and conventional logging (CL, without a management plan) on physical and biochemical characteristics of Ferralsol soils that developed on pre-Cambrian rocks in rainforests of Cameroon. Five to seven months after the logging operations were completed, we mapped the CL and RIL sites and quantified the disturbed areas: felling gaps, skidding trails, logging decks and roads. We selected four replicate plots at each site that encompassed these four disturbed strata and an adjacent undisturbed area as the reference. At each disturbed stratum and reference area per plot, we took soil samples down to 50 cm, and quantified soil physical and biochemical characteristics. Nutrient exports with timber harvest were also quantified. The logging intensity was very low with removals of 0.2 and 0.3 tree per hectare, and the ground area disturbed accounted only 5.2% and 4.0% of the total area in CL and RIL, respectively. In terms of area disturbance for each harvested tree, CL had 753 m 2 tree −1 more affected ground area than RIL. Roads and logging decks were the most affected by logging operations, where effective cation exchange capacity, soil organic carbon (SOC), total nitrogen (N), Bray-extractable phosphorus (P) and exchangeable aluminum decreased whereas pH, 15 N natural abundance and exchangeable manganese increased compared to the undisturbed reference area (P < 0.01-0.04). The disturbed area showed overall reductions of 21-29% in SOC, N and P stocks relative to the reference areas (P = 0.02-0.07). The amounts of C, N, P and base cations exported with harvested timber were only 0.4-5.9% of the changes in stocks of these elements in the disturbed strata. Nutrient reductions in the soil and exports through timber harvest were comparable between CL and RIL, after one logging event in this very low intensity logging systems. Our results suggest that unplanned operations together with frequent re-logging inherent to CL can increase area damage and enhance changes in SOC and nutrients as opposed to RIL, which may affect the recovery of the succeeding vegetation."],["dc.identifier.doi","10.1016/j.foreco.2019.117522"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/62756"],["dc.language.iso","en"],["dc.relation.issn","0378-1127"],["dc.title","Changes in soil organic carbon and nutrient stocks in conventional selective logging versus reduced-impact logging in rainforests on highly weathered soils in Southern Cameroon"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","59"],["dc.bibliographiccitation.issue","1"],["dc.bibliographiccitation.journal","Nutrient Cycling in Agroecosystems"],["dc.bibliographiccitation.lastpage","79"],["dc.bibliographiccitation.volume","124"],["dc.contributor.author","Quiñones, Cecille Marie O."],["dc.contributor.author","Veldkamp, Edzo"],["dc.contributor.author","Lina, Suzette B."],["dc.contributor.author","Bande, Marlito Jose M."],["dc.contributor.author","Arribado, Arwin O."],["dc.contributor.author","Corre, Marife D."],["dc.date.accessioned","2022-09-01T09:49:21Z"],["dc.date.available","2022-09-01T09:49:21Z"],["dc.date.issued","2022"],["dc.description.abstract","Abstract\n \n Field-based quantification of soil greenhouse gas emissions from the Philippines’ agriculture sector is missing for vegetable production systems, despite its substantial contribution to agricultural production. We quantified soil N\n 2\n O emission, CH\n 4\n uptake, and CO\n 2\n efflux in vegetable farms and compared these to the secondary forest. Measurements were conducted for 13 months in 10 smallholder farms and nine forest plots on Andosol soil in Leyte, Philippines using static chambers. Soil N\n 2\n O and CO\n 2\n emissions were higher, whereas CH\n 4\n uptake was lower in the vegetable farms than in the forest. Vegetable farms had annual fluxes of 12.7 ± 2.6 kg N\n 2\n O-N ha\n −1\n  yr\n −1\n , −1.1 ± 0.2 kg CH\n 4\n -C ha\n −1\n  yr\n −1\n , and 11.7 ± 0.7 Mg CO\n 2\n -C ha\n −1\n  yr\n −1\n , whereas the forest had 0.10 ± 0.02 kg N\n 2\n O-N ha ha\n −1\n  yr\n −1\n , −2.0 ± 0.2 kg CH\n 4\n -C ha\n −1\n  yr\n −1\n , and 8.2 ± 0.7 Mg CO\n 2\n -C ha\n −1\n  yr\n −1\n . Long-term high N fertilization rates in vegetable farms resulted in large soil mineral N levels, dominated by NO\n 3\n –\n in the topsoil and down to 1-m depth, leading to high soil N\n 2\n O emissions. Increased soil bulk density in the vegetable farms probably increased anaerobic microsites during the wet season and reduced CH\n 4\n diffusion from the atmosphere into the soil, resulting in decreased soil CH\n 4\n uptake. High soil CO\n 2\n emissions from the vegetable farms suggested decomposition of labile organic matter, possibly facilitated by plowing and large N fertilization rates. The global warming potential of these vegetable farms was 31 ± 2.7 Mg CO\n 2\n -eq ha\n −1\n  yr\n −1\n (100-year time frame)."],["dc.identifier.doi","10.1007/s10705-022-10222-4"],["dc.identifier.pii","10222"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/113399"],["dc.language.iso","en"],["dc.notes.intern","DOI-Import GROB-597"],["dc.relation.eissn","1573-0867"],["dc.relation.issn","1385-1314"],["dc.rights.uri","https://creativecommons.org/licenses/by/4.0"],["dc.title","Soil greenhouse gas fluxes from tropical vegetable farms, using forest as a reference"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","3802"],["dc.bibliographiccitation.issue","12"],["dc.bibliographiccitation.journal","Global Change Biology"],["dc.bibliographiccitation.lastpage","3813"],["dc.bibliographiccitation.volume","20"],["dc.contributor.author","Matson, Amanda L."],["dc.contributor.author","Corre, Marife D."],["dc.contributor.author","Veldkamp, Edzo"],["dc.date.accessioned","2017-09-07T11:43:42Z"],["dc.date.available","2017-09-07T11:43:42Z"],["dc.date.issued","2014"],["dc.identifier.doi","10.1111/gcb.12668"],["dc.identifier.gro","3150204"],["dc.identifier.pmid","24965673"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/6943"],["dc.language.iso","en"],["dc.notes.status","zu prüfen"],["dc.relation.issn","1354-1013"],["dc.title","Nitrogen cycling in canopy soils of tropical montane forests responds rapidly to indirect N and P fertilization"],["dc.type","journal_article"],["dc.type.internalPublication","unknown"],["dc.type.peerReviewed","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","740"],["dc.bibliographiccitation.issue","3"],["dc.bibliographiccitation.journal","Soil Biology and Biochemistry"],["dc.bibliographiccitation.lastpage","750"],["dc.bibliographiccitation.volume","40"],["dc.contributor.author","Sotta, Eleneide Doff"],["dc.contributor.author","Corre, Marife D."],["dc.contributor.author","Veldkamp, Edzo"],["dc.date.accessioned","2017-09-07T11:43:34Z"],["dc.date.available","2017-09-07T11:43:34Z"],["dc.date.issued","2007"],["dc.identifier.doi","10.1016/j.soilbio.2007.10.009"],["dc.identifier.gro","3150179"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/6915"],["dc.language.iso","en"],["dc.notes.status","zu prüfen"],["dc.relation.issn","0038-0717"],["dc.title","Differing N status and N retention processes of soils under old-growth lowland forest in Eastern Amazonia, Caxiuanã, Brazil"],["dc.type","journal_article"],["dc.type.internalPublication","unknown"],["dc.type.peerReviewed","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","2049"],["dc.bibliographiccitation.issue","8"],["dc.bibliographiccitation.journal","Global Change Biology"],["dc.bibliographiccitation.lastpage","2066"],["dc.bibliographiccitation.volume","15"],["dc.contributor.author","Koehler, Birgit"],["dc.contributor.author","Corre, Marife D."],["dc.contributor.author","Veldkamp, Edzo"],["dc.contributor.author","Wullaert, Hans"],["dc.contributor.author","Wright, S. Joseph"],["dc.date.accessioned","2021-12-08T12:27:48Z"],["dc.date.available","2021-12-08T12:27:48Z"],["dc.date.issued","2009"],["dc.description.abstract","Tropical nitrogen (N) deposition is projected to increase substantially within the coming decades. Increases in soil emissions of the climate-relevant trace gases NO and N2O are expected, but few studies address this possibility. We used N addition experiments to achieve N-enriched conditions in contrasting montane and lowland forests and assessed changes in the timing and magnitude of soil N-oxide emissions. We evaluated transitory effects, which occurred immediately after N addition, and long-term effects measured at least 6 weeks after N addition. In the montane forest where stem growth was N limited, the first-time N additions caused rapid increases in soil N-oxide emissions. During the first 2 years of N addition, annual N-oxide emissions were five times (transitory effect) and two times (long-term effect) larger than controls. This contradicts the current assumption that N-limited tropical montane forests will respond to N additions with only small and delayed increases in soil N-oxide emissions. We attribute this fast and large response of soil N-oxide emissions to the presence of an organic layer (a characteristic feature of this forest type) in which nitrification increased substantially following N addition. In the lowland forest where stem growth was neither N nor phosphorus (P) limited, the first-time N additions caused only gradual and minimal increases in soil N-oxide emissions. These first N additions were completed at the beginning of the wet season, and low soil water content may have limited nitrification. In contrast, the 9- and 10-year N-addition plots displayed instantaneous and large soil N-oxide emissions. Annual N-oxide emissions under chronic N addition were seven times (transitory effect) and four times (long-term effect) larger than controls. Seasonal changes in soil water content also caused seasonal changes in soil N-oxide emissions from the 9- and 10-year N-addition plots. This suggests that climate change scenarios, where rainfall quantity and seasonality change, will alter the relative importance of soil NO and N2O emissions from tropical forests exposed to elevated N deposition."],["dc.identifier.doi","10.1111/j.1365-2486.2008.01826.x"],["dc.identifier.gro","3150159"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/95455"],["dc.language.iso","en"],["dc.notes.intern","DOI-Import GROB-476"],["dc.notes.status","public"],["dc.relation.eissn","1365-2486"],["dc.relation.issn","1354-1013"],["dc.rights.uri","http://doi.wiley.com/10.1002/tdm_license_1.1"],["dc.subject","climate change; deposition; fertilization; nitric oxide; nitrification; nitrogen; nitrous oxide; organic layer; trace gases; tropical forest"],["dc.title","Immediate and long-term nitrogen oxide emissions from tropical forest soils exposed to elevated nitrogen input"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","no"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.issue","2"],["dc.bibliographiccitation.journal","AGRIVITA"],["dc.bibliographiccitation.volume","40"],["dc.contributor.author","Kurniawan, Syahrul"],["dc.contributor.author","Corre, Marife D."],["dc.contributor.author","Utami, Sri Rahayu"],["dc.contributor.author","Veldkamp, Edzo"],["dc.date.accessioned","2020-12-10T18:42:48Z"],["dc.date.available","2020-12-10T18:42:48Z"],["dc.date.issued","2018"],["dc.identifier.doi","10.17503/agrivita.v40i2.1723"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/78089"],["dc.notes.intern","DOI Import GROB-354"],["dc.relation","SFB 990: Ökologische und sozioökonomische Funktionen tropischer Tieflandregenwald-Transformationssysteme (Sumatra, Indonesien)"],["dc.relation","SFB 990 | A | A05: Optimierung des Nährstoffmanagements in Ölpalmplantagen und Hochrechnung plot-basierter Treibhausgasflüsse auf die Landschaftsebene transformierter Regenwälder"],["dc.subject.gro","sfb990_journalarticles"],["dc.title","Soil Biochemical Properties and Nutrient Leaching from Smallholder Oil Palm Plantations, Sumatra-Indonesia"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.subtype","original_ja"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","749"],["dc.bibliographiccitation.issue","3"],["dc.bibliographiccitation.journal","Ecology"],["dc.bibliographiccitation.lastpage","761"],["dc.bibliographiccitation.volume","96"],["dc.contributor.author","Baldos, Angelica P."],["dc.contributor.author","Corre, Marife D."],["dc.contributor.author","Veldkamp, Edzo"],["dc.date.accessioned","2017-09-07T11:43:39Z"],["dc.date.available","2017-09-07T11:43:39Z"],["dc.date.issued","2015"],["dc.description.abstract","Large areas in the tropics receive elevated atmospheric nutrient inputs. Presently, little is known on how nitrogen (N) cycling in tropical montane forest soils will respond to such increased nutrient inputs. We assessed how gross rates of mineral N production (N mineralization and nitrification) and microbial N retention (NH4+ and NO3− immobilization and dissimilatory NO3− reduction to NH4+ [DNRA]) change with elevated N and phosphorus (P) inputs in montane forest soils at 1000-, 2000-, and 3000-m elevations in south Ecuador. At each elevation, four replicate plots (20 × 20 m each) of control, N (added at 50 kg N·ha−1·yr−1), P (added at 10 kg P·ha−1·yr−1), and combined N + P additions have been established since 2008. We measured gross N cycling rates in 2010 and 2011, using 15N pool dilution techniques with in situ incubation of intact soil cores taken from the top 5 cm of soil. In control plots, gross soil-N cycling rates decreased with increase in elevation, and microbial N retention was tightly coupled with mineral N production. At 1000 m and 2000 m, four-year N and combined N + P additions increased gross mineral N production but decreased NH4+ and NO3− immobilization and DNRA compared to the control. At 3000 m, four-year N and combined N + P additions increased gross N mineralization rates and decreased DNRA compared to the control; although NH4+ and NO3− immobilization in the N and N + P plots were not different from the control, these were lower than their respective mineral N production. At all elevations, decreased microbial N retention was accompanied by decreased microbial biomass C and C:N ratio. P addition did not affect any of the soil-N cycling processes. Our results signified that four years of N addition, at a rate expected to occur at these sites, uncoupled the soil-N cycling processes, as indicated by decreased microbial N retention. This fast response of soil-N cycling processes across elevations implies that greater attention should be paid to the biological implications on montane forests of such uncoupled soil-N cycling."],["dc.identifier.doi","10.1890/14-0295.1"],["dc.identifier.gro","3150196"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/6934"],["dc.language.iso","en"],["dc.notes.status","public"],["dc.relation.issn","0012-9658"],["dc.subject","dissimilatory nitrate reduction to ammonium; gross N mineralization; gross nitrification; microbial N immobilization;nitrogen and phosphorus additions; nutrient manipulation experiment; tropical Andes ;tropical montane forests"],["dc.title","Response of N cycling to nutrient inputs in forest soils across a 1000–3000 m elevation gradient in the Ecuadorian Andes"],["dc.type","journal_article"],["dc.type.internalPublication","unknown"],["dc.type.peerReviewed","no"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","26"],["dc.bibliographiccitation.journal","Forest Ecology and Management"],["dc.bibliographiccitation.lastpage","33"],["dc.bibliographiccitation.volume","313"],["dc.contributor.author","Blécourt, Marleen de"],["dc.contributor.author","Hänsel, Vera Maria"],["dc.contributor.author","Brumme, Rainer"],["dc.contributor.author","Corre, Marife D."],["dc.contributor.author","Veldkamp, Edzo"],["dc.date.accessioned","2017-09-07T11:54:54Z"],["dc.date.available","2017-09-07T11:54:54Z"],["dc.date.issued","2013"],["dc.description.abstract","Secondary forest-to-rubber (Hevea brasiliensis) plantation conversion is an important recent land-use change in the montane regions of mainland Southeast Asia. This land-use conversion caused a reduction of soil organic carbon (SOC) stocks by on average 19% down to 1.2 m over 46 years. Due to the mountainous topography of the region, most rubber plantations include narrow terraces parallel to contours. Manual terrace construction involves cutting of the soil from the upper slope and piling up the removed soil on the soil surface downslope. Soil redistribution by terrace construction may affect SOC dynamics through exposure of the subsurface soil at the terrace inner sides (cut section) and soil burial at the terrace outer edges (fill section).Our study, conducted in southern Yunnan province of China, aimed to quantify SOC stock changes induced by terrace construction. In three rubber plantations aged 5, 29 and 44 years, we systematically sampled the terraces according to soil redistribution zones, and the original sloping areas in between the terraces were used as reference.At the cut section of the terrace, topsoil removal caused a depletion of SOC stocks in the youngest plantation followed by SOC stock recovery in the two oldest plantations. The recovery of SOC stocks at the cut section in the two oldest plantations was attributed to the capacity of the exposed subsurface soil to store new organic carbon inputs from roots and litter, and to sedimentation of eroded topsoil materials from the upper slope. At the fill section of the terrace, soil deposition resulted in higher total SOC stocks compared to the reference position in all plantations. This was due to the deposition of redistributed soil material on top of the original soil surface combined with the partial preservation of carbon in the buried soil. Overall, the increase of SOC in the exposed subsurface soil at the cut sections, and the partial preservation of SOC in the buried soil at the fill sections resulted in higher SOC stocks down to 1.2 m at the terraces compared to the reference positions in the two oldest plantations. Our results imply that terracing may alleviate SOC losses caused by the conversion of secondary forest to terraced rubber plantation."],["dc.identifier.doi","10.1016/j.foreco.2013.10.043"],["dc.identifier.gro","3150143"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/6874"],["dc.language.iso","en"],["dc.notes.status","public"],["dc.relation.issn","0378-1127"],["dc.title","Soil redistribution by terracing alleviates soil organic carbon losses caused by forest conversion to rubber plantation"],["dc.type","journal_article"],["dc.type.internalPublication","unknown"],["dc.type.peerReviewed","no"],["dspace.entity.type","Publication"]]