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1.
PLoS One ; 15(2): e0228717, 2020.
Article in English | MEDLINE | ID: mdl-32027704

ABSTRACT

Conservation farming (CF), involving basin tillage, residue retention and crop rotation, combined with biochar may help to mitigate negative impacts of conventional agriculture. In this study, the effects of CF on the amount and quality of soil organic matter (SOM) and potential nitrogen (N) mineralization were investigated in a maize-soya-maize rotation in an Acrisol in Zambia. A large field was run under CF for 7 years and in the subsequent three growing seasons (2015-2018), four management practices were introduced to study effects on soil characteristics and crop yield. We tested i) a continuation of regular CF (CF-NORM) ii) CF without residue retention (CF-NO-RES); iii) Conventional (CONV), with full tillage and removal of residues; and iv) CF with 4 ton ha-1 pigeon pea biochar inside basins and residue retention (CF-BC). The experiment involved the addition of fertilizer only to maize, while soya received none. Soya yield was significantly higher in CF systems than in CONV. Maize yields were not affected by the different management practices probably due to the ample fertilizer addition. CF-NORM had a higher stock of soil organic carbon (SOC), higher N mineralization rates, more hot-water extractable carbon (HWEC; labile SOC) and particulate organic matter (POM) inside basins compared to the surrounding soil (outside basins). Our results suggest that the input of roots inside basins are more effective increasing SOM and N mineralization, than the crop residues that are placed outside basins. CONV reduced both quality and quantity of SOM and N mineralization as compared to CF inside basins. CF-BC increased the amount of SOC as compared with CF-NORM, whereas N mineralization rate and HWEC remained unaffected. The results suggest benefits on yield of CF and none of biochar; larger impact of root biomass on the build-up of SOM than crop residues; and high stability of biochar in soil.


Subject(s)
Agriculture/methods , Carbon/analysis , Charcoal/pharmacology , Crops, Agricultural/growth & development , Minerals/chemistry , Nitrogen/chemistry , Soil/chemistry , Biomass , Conservation of Natural Resources , Crops, Agricultural/drug effects , Humidity
2.
Ecol Evol ; 8(1): 462-476, 2018 01.
Article in English | MEDLINE | ID: mdl-29321886

ABSTRACT

Stand dynamics and the gap initiation prior to gap formation are not well-understood because of its long-term nature and the scarcity of late-successional stands. Reconstruction of such disturbance is normally based on historical records and dendroecological methods. We investigated gap initiation and formation at the fine-scale stand level in the old-growth reserve of Karlshaugen in Norway. Given its long-term conservation history, and thorough mapping in permanent marked plots with spatially referenced trees, it provides an opportunity to present stand development before, during, and after gap formation. Late-successional decline in biomass was recorded after more than 50 years of close to steady state. Gaps in the canopy were mainly created by large old trees that had been killed by spruce bark beetles. Snapping by wind was the main reason for treefall. Long-term dominance of Norway spruce excluded downy birch and Scots pine from the stand. Comparisons of the forest floor soil properties between the gap and nongap area showed significantly higher concentrations of plant available Ca within the gap area. Plant root simulator (PRS™) probes showed significantly higher supply rates for Ca and Mg, but significantly lower K for the gap compared to the nongap area. Soil water from the gap area had significantly higher C:N ratios compared to the nongap area. Fine-scale variation with increasing distance to logs indicated that CWD is important for leaking of DOC and Ca. Our long-term study from Karlshaugen documents gap dynamics after more than 50 years of steady state and a multiscale disturbance regime in an old-growth forest. The observed disturbance dynamic caused higher aboveground and belowground heterogeneity in plots, coarse woody debris, and nutrients. Our study of the nutrient levels of the forest floor suggest that natural gaps of old-growth forest provide a long-lasting biogeochemical feedback system particularly with respect to Ca and probably also N. Norway spruce trees near the gap edge responded with high plasticity to reduced competition, showing the importance of the edge zone as hot spots for establishing heterogeneity, but also the potential for carbon sequestration in old-growth forest.

3.
J Agric Food Chem ; 62(17): 3791-9, 2014 Apr 30.
Article in English | MEDLINE | ID: mdl-24720814

ABSTRACT

Biochar properties vary, and characterization of biochars is necessary for assessing their potential to sequester carbon and improve soil functions. This study aimed at assessing key surface properties of agronomic relevance for products from slow pyrolysis at 250-800 °C, hydrothermal carbonization (HTC), and flash carbonization. The study further aimed at relating surface properties to current characterization indicators. The results suggest that biochar chemical composition can be inferred from volatile matter (VM) and is consistent for corncob and miscanthus feedstocks and for the three tested production methods. High surface area was reached within a narrow temperature range around 600 °C, whereas cation exchange capacity (CEC) peaked at lower temperatures. CEC and pH values of HTC chars differed from those of slow pyrolysis biochars. Neither CEC nor surface area correlated well with VM or atomic ratios. These results suggest that VM and atomic ratios H/C and O/C are good indicators of the degree of carbonization but poor predictors of the agronomic properties of biochar.


Subject(s)
Charcoal/chemistry , Hydrogen-Ion Concentration , Surface Properties , Temperature
4.
ISRN Nurs ; 2011: 208142, 2011.
Article in English | MEDLINE | ID: mdl-22013540

ABSTRACT

Background. Nursing homes face challenges in the coming years due to the increased number of elderly. Quality will be under pressure, expectations of the services will rise, and clinical complexity will grow. New strategies are needed to meet this situation. Modern clinical information systems with decision support may be part of that. Objectives. To study the impact of introducing an electronic patient record system with decision support on the use of warfarin, neuroleptics and weighing of patients, in nursing homes. Methods. A prevalence study was performed in seven nursing homes with 513 subjects. A before-after study with internal controls was performed. Results. The prevalence of atrial fibrillation in the seven nursing homes was 18.8%. After intervention, the proportion of all patients taking warfarin increased from 3.0% to 9.8% (P = 0.0086), neuroleptics decreased from 33.0% to 21.5% (P = 0.0121), and the proportion not weighed decreased from 72.6% to 16.0% (P < 0.0001). The internal controls did not change significantly. Conclusion. Statistics and management data can be continuously produced to monitor the quality of work processes. The electronic health record system and its system for decision support can improve drug therapy and monitoring of treatment policy.

5.
Biochemistry ; 48(25): 5785-93, 2009 Jun 30.
Article in English | MEDLINE | ID: mdl-19445480

ABSTRACT

Aquaporin-4 (AQP4) is a water channel found at high concentrations around blood vessels in the brain and is organized into elaborate assemblies called square arrays. The natural functions of AQP4 and the square arrays remain unknown, but under pathophysiological conditions, AQP4 has been shown to influence brain edema, synapse function, and cellular migration. AQP4 was recently found to have six isoforms, where AQP4a (also known as M1), AQP4c (also known as M23), and AQP4e are functional water transport channels. Furthermore, by two-dimensional blue native polyacrylamide gel electrophoresis (BN-PAGE) analysis of the internal composition of square arrays, three distinct isoforms were visualized. Here we combine these advances in technique with mutational analysis to test a series of current hypotheses about AQP4 functional structure. We find that the square array destabilizing N-terminus of AQP4a is partly functional through the C13 and C17 amino acids, and not through R8 and R9. We find a discrepancy between our data and the proposed tetramer-tetramer binding site based on the in vitro AQP4 two-dimensional crystal structure. On the other hand, we find that isoforms AQP4a and AQP4e, while not being able to form square arrays alone, are able to interact with AQP4c and be incorporated into higher-order structures. Our results with the novel BN-PAGE analysis technique point toward a model in which the presence of accessory isoforms (AQP4a and AQP4e) regulates the square array assembly process of the main isoform, AQP4c.


Subject(s)
Aquaporin 4/chemistry , Aquaporin 4/physiology , Amino Acid Sequence , Aquaporin 4/genetics , Freeze Fracturing , HeLa Cells , Humans , Molecular Sequence Data , Mutation , Peptide Fragments/chemistry , Peptide Fragments/genetics , Peptide Fragments/physiology , Protein Isoforms/chemistry , Protein Isoforms/genetics , Protein Isoforms/physiology
6.
Ambio ; 37(1): 18-28, 2008 Feb.
Article in English | MEDLINE | ID: mdl-18341114

ABSTRACT

To provide baseline data for climate manipulation experiments in 11 small (30-268 m2) headwater catchments at Storgama, Telemark County, Southern Norway, we assessed the natural variability in site characteristics and runoff quality. Annual average concentrations in runoff at the sites have coefficients of variation between 26-61%, with the smallest values for total organic carbon (TOC) and carbon to nitrogen (C/N) ratios and the largest for inorganic nitrogen (N). The catchments have between two and five times higher concentrations of inorganic N, TOC, and total phosphorus than the larger (0.6 km2) Storgama watershed nearby. Concentrations of TOC and TON in runoff tend to increase with soil C and N content and with the volume of soil in the catchment. For nitrate (NO3) and ammonium in runoff, the reverse is true. In wet years the proportion of bare rock is a major predictor for the annual average NO3 concentration in runoff.


Subject(s)
Carbon/analysis , Nitrogen/analysis , Soil Pollutants/analysis , Water Pollutants, Chemical/analysis , Air Pollution , Chemical Precipitation , Ecosystem , Models, Theoretical , Nitrates/analysis , Norway , Seasons
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