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Data from: Leaf hydraulic parameters are more plastic in species that experience a wider range of leaf water potentials
负责人:
关键词:
turgor;isohydry;transpiration;drought;Embolism;pressure-volume curves
DOI:
doi:10.5061/dryad.vb188
摘要:
1. Many plant species experience large differences in soil moisture availability within a season, potentially leading to a wide range
Data from: CO2 enrichment and soil type additively regulate grassland productivity
负责人:
关键词:
soil water potential;Soil texture;rangeland;subambient CO2 concentration.;atmospheric CO2 enrichment;aboveground productivity;species composition
DOI:
doi:10.5061/dryad.1hc582s
摘要:
differs among ecosystems. Soil properties affect ANPP via multiple mechanisms and vary over topographic to geographic gradients, but have received littl
Data from: The role of soil chemistry and plant neighbourhoods in structuring fungal communities in three Panamanian rainforests
负责人:
关键词:
Metabarcoding;Plant\u2013soil (below-ground) interactions;Panama;mycorrhizal fungi;ITS1;microbial ecology;soil phosphorus
DOI:
doi:10.5061/dryad.sc38s
摘要:
). Linear models showed that AM OTU richness was not explained by any independent variable. For non-AM fungi, phosphorus, pH, and soil moisture better predicted OTU
Data from: Broad-scale patterns of soil carbon (C) pools and fluxes across semiarid ecosystems are linked to climate and soil texture
负责人:
关键词:
dryland ecosystems;microbial biomass;soil organic carbon;climate;clay
DOI:
doi:10.5061/dryad.7r3742r
摘要:
. Our study revealed a high degree of collinearity among C stocks and fluxes, which were related to climate, vegetation, and soil clay content. Soil C pools wer
Data from: Development and calibration of a novel sensor to quantify the water content of surface soils and biological soil crusts
负责人:
关键词:
wetness probe;humidity sensor;nitrogen cycling;biogeochemical cycle;carbon balance;biocrusts;electrical conductivity;calibration;precipitation equivalent;physiological activity
DOI:
doi:10.5061/dryad.605j6
摘要:
of the water content of both bare and crusted soils are thus urgently needed to correctly model the exchange processes of water, nutrients and trace gases
Data from: The influence of soil communities on the temperature sensitivity of soil respiration
负责人:
关键词:
Metabolic Rate;Boreal forest;Temperature sensitivity;Tropical Forest;Soil community;Population abundance;soil respiration;Individual mass;biome;Soil biota;tundra;Temperate Forest;Temperate grassland
DOI:
doi:10.5061/dryad.416kv03
摘要:
Soil respiration represents a major carbon flux between terrestrial ecosystems and the atmosphere, and is expected to accelerate under
Data from: The extension of internal humidity levels beyond the soil surface facilitates mound expansion in Macrotermes
负责人:
关键词:
humidity;construction;Macrotermes;Termite;Self-organization;Mound
DOI:
doi:10.5061/dryad.xd2547ddr
摘要:
and depositing soil at its edge. Such deposition of additional moist soil will increase local humidity, in a feedback loop allowing the “interior” zone to progress
Data from: Aggregation but not organo-metal complexes contributed to C storage in tidal freshwater wetland soils
负责人:
关键词:
soil carbon;tidal freshwater wetlands;aggregates
DOI:
doi:10.5061/dryad.hr67c5p
摘要:
One of the many goals of wetland restoration is to promote the long-term storage of carbon (C) in the terrestrial biosphere. Unfortunately, soil
Data from: Large, climate-sensitive soil carbon stocks mapped with pedology-informed machine learning in the North Pacific
负责人:
关键词:
Anthropocene;soil carbon;pedology;Random Forest;Machine Learning;Holocene;temperate rainforest
DOI:
doi:10.5061/dryad.5jf6j1r
摘要:
soil moisture. The random forest model predicted stocks of 4.5 Pg C (to 1 m) for the study region, 22% of which was stored in organic soil layers. Calculated
Data from: Hotspots of soil N2O emission enhanced through water absorption by plant residue
负责人:
关键词:
15N site preference;2D oxygen mapping;pore size distribution;arable soil;computed micro-tomography
DOI:
doi:10.5061/dryad.83150
摘要:
: water absorption by plant residue that creates unique micro-environmental conditions, markedly different from those of the bulk soil. Moisture levels

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