Interpreting, Measuring, and Modeling Soil Respiration
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Foliar and Ecosystem Respiration in an Old-Growth Tropical Rain Forest
Plant, Cell and Environment (2008) 31, 473–483 doi: 10.1111/j.1365-3040.2008.01775.x Foliar and ecosystem respiration in an old-growth tropical rain forest MOLLY A. CAVALERI1,2, STEVEN F. OBERBAUER3,4 & MICHAEL G. RYAN5,6 1Graduate Degree Program in Ecology, Colorado State University, Fort Collins, CO 80523, USA, 2Botany Department, University of Hawaii, Manoa, 3190 Maile Way, Honolulu, HI 96826, USA, 3Department of Biological Sciences, Florida International University, 11200 SW 8th Street, Miami, FL 33199, USA, 4Fairchild Tropical Botanic Garden, 11935 Old Cutler Road, Miami, FL 33156, USA, 5United States Department of Agriculture Forest Service, Rocky Mountain Research Station, 240 West Prospect RD, Fort Collins, CO 80526, USA and 6Graduate Degree Program in Ecology, Department of Forest, Rangeland, and Watershed Stewardship, Colorado State University, Fort Collins, CO 80523, USA ABSTRACT Chambers et al. 2004). Results vary widely about whether tropical forests are presently acting as carbon sources or Foliar respiration is a major component of ecosystem res- sinks, or how this may be affected by global warming. piration, yet extrapolations are often uncertain in tropical Several eddy flux studies have concluded that tropical rain forests because of indirect estimates of leaf area index forests are primarily acting as carbon sinks (Fan et al. 1990; (LAI). A portable tower was used to directly measure LAI Grace et al. 1995; Malhi et al. 1998; Loescher et al. 2003, and night-time foliar respiration from 52 vertical transects but see Saleska et al. 2003). Many atmosphere–biosphere throughout an old-growth tropical rain forest in Costa Rica. modelling studies, on the other hand, predict that tropical In this study, we (1) explored the effects of structural, func- forests will be an increased carbon source with global tional and environmental variables on foliar respiration; (2) warming (Kindermann, Würth & Kohlmaier 1996; Braswell extrapolated foliar respiration to the ecosystem; and (3) et al. -
Fact Sheet 3: Organic Matter Decline
Sustainable agriculture and soil conservation Soil degradation processes Fact sheet no. 3 Organic matter decline What is organic matter decline? Soil organic matter includes all living soil organisms together with the remains of dead organisms in their various degrees of decomposition. The organic carbon content of a soil is made up of heterogeneous mixtures of both simple and complex substances containing carbon. The sources for organic matter are crop residues, animal and green manures, compost and other organic materials. A decline in organic matter is caused by the reduced presence of decaying organisms, or an increased rate of decay as a result of changes in natural or anthropogenic factors. Organic matter is regarded as a vital component of a healthy soil; its decline results in a soil that is degraded. A soil that is rich in organic matter (Source: Soil Atlas of Europe) Why is soil organic matter/carbon important? Soil organic matter is a source of food for soil fauna, and contributes to soil biodiversity by acting as a reservoir of soil nutrients such as nitrogen, phosphorus and sulphur; it is the main contributor to soil fertility. Soil organic carbon supports the soil’s structure, improving the physical environment for roots to penetrate through the soil. Organic matter absorbs water – it is able to hold about six times its weight in water – making it a lifeline for vegetation in naturally dry and sandy soils. Soils containing organic matter have a better structure that improves water infiltration, and reduces the soil’s susceptibility to compaction, erosion, desertification and landslides. On a global scale, soils contain around twice the amount of carbon held in the atmosphere and three times the amount found in vegetation. -
Effects of Nitrogen Additions on Soil Respiration in an Asian Tropical Montane Rainforest
Article Effects of Nitrogen Additions on Soil Respiration in an Asian Tropical Montane Rainforest Fangtao Wu 1,2, Changhui Peng 1,2,3,* , Weiguo Liu 1,2, Zhihao Liu 1,2, Hui Wang 1,2, Dexiang Chen 4 and Yide Li 4 1 Center for Ecological Forecasting and Global Change, College of Forestry, Northwest A&F University, Yangling 712100, China; [email protected] (F.W.); [email protected] (W.L.); [email protected] (Z.L.); [email protected] (H.W.) 2 State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Northwest A&F University, Yangling 712100, China 3 Department of Biology Sciences, Institute of Environment Sciences, University of Quebec at Montreal, C.P. 8888, Succ. Centre-Ville, Montreal, QC H3C 3P8, Canada 4 Jianfengling National Key Field Observation and Research Station for Forest Ecosystem, Research Institute of Tropical Forestry, Chinese Academy of Forestry, Guangzhou 510520, China; [email protected] (D.C.); [email protected] (Y.L.) * Correspondence: [email protected] Abstract: Understanding the impacts of nitrogen (N) addition on soil respiration (RS) and its temper- ature sensitivity (Q10) in tropical forests is very important for the global carbon cycle in a changing environment. Here, we investigated how RS respond to N addition in a tropical montane rainforest in Southern China. Four levels of N treatments (0, 25, 50, and 100 kg N ha−1 a−1 as control (CK), low N (N25), moderate N (N50), and high N (N100), respectively) were established in September 2010. Based on a static chamber-gas chromatography method, R was measured from January 2015 S to December 2018. -
Soils and Fertilizers for Master Gardeners: Soil Organic Matter and Organic Amendments1 Gurpal S
SL273 Soils and Fertilizers for Master Gardeners: Soil Organic Matter and Organic Amendments1 Gurpal S. Toor, Amy L. Shober, and Alexander J. Reisinger2 This article is part of a series entitled Soils and Fertilizers for Master Gardeners. The rest of the series can be found at http://edis.ifas.ufl.edu/topic_series_soils_and_fertil- izers_for_master_gardeners. A glossary can also be found at http://edis.ifas.ufl.edu/MG457. Introduction and Purpose Organic matter normally occupies the smallest portion of the soil physical makeup (approximately 5% of total soil volume on average, and usually 1 to 3% for Florida’s sandy soils) but is the most dynamic soil component (Figure Figure 1. Typical components of soil. 1). The primary sources of soil organic matter are plant Credits: Gurpal Toor and animal residues. Soil organic matter is important for maintaining good soil structure, which enhances the What is the composition of soil movement of air and water in soil. Organic matter also organic matter? plays an important role in nutrient cycling. This publication is designed to educate homeowners about the importance Soil organic matter contains (i) living biomass: plant, of soil organic matter and provide suggestions about how to animal tissues, and microorganisms; (ii) dead tissues: partly build the organic matter in garden and landscape soils. decomposed materials; and (iii) non-living materials: stable portion formed from decomposed materials, also known as humus. Soil organic matter typically contains about 50% carbon. The remainder of soil organic matter consists of about 40% oxygen, 5% hydrogen, 4% nitrogen, and 1% sulfur. The amount of organic matter in soils varies widely, from 1 to 10% (total dry weight) in most soils to more than 90% in organic (muck) soils. -
Effects of Wheel Traffic and Farmyard Manure Applications on Soil CO2
Turkish Journal of Agriculture and Forestry Turk J Agric For (2018) 42: 288-297 http://journals.tubitak.gov.tr/agriculture/ © TÜBİTAK Research Article doi:10.3906/tar-1709-79 Effects of wheel traffic and farmyard manure applications on soil CO2 emission and soil oxygen content 1, 1 2 Sefa ALTIKAT *, H. Kaan KÜÇÜKERDEM , Aysun ALTIKAT 1 Department of Biosystem Engineering, Faculty of Agriculture, Iğdır University, Iğdır, Turkey 2 Department of Environmental Engineering, Faculty of Engineering, Iğdır University, Iğdır, Turkey Received: 20.09.2017 Accepted/Published Online: 17.04.2018 Final Version: 07.08.2018 Abstract: This 2-year field study investigated the effects of different wheel traffic passes, manure amounts, and manure application methods on soil temperature, soil moisture, CO2 emission, and soil O2 content. To achieve this purpose, three different wheel traffic applications (no traffic, one pass, and two passes) were used. In the experiments, two different methods of manure applications (surface and subsurface) and three different farmyard manure amounts were used with a control plot (N0), 40 Mg ha–1 (N40), and 80 Mg ha–1 (N80). Manure was applied in both years of the experiment in the first week of April. For the subsurface application, the manure was mixed in at approximately 10 cm of soil depth with a rotary tiller. According to the results, soil temperature, soil moisture, penetration resistance, and bulk density increased with increasing wheel traffic except 2CO emission for 2014 and 2015. CO2 emission values decreased with traffic. Subsurface manure application caused more 2CO emission compared to surface application. The increase in manure amounts led to an increase in CO2 emission and soil moisture content. -
Agricultural Soil Compaction: Causes and Management
October 2010 Agdex 510-1 Agricultural Soil Compaction: Causes and Management oil compaction can be a serious and unnecessary soil aggregates, which has a negative affect on soil S form of soil degradation that can result in increased aggregate structure. soil erosion and decreased crop production. Soil compaction can have a number of negative effects on Compaction of soil is the compression of soil particles into soil quality and crop production including the following: a smaller volume, which reduces the size of pore space available for air and water. Most soils are composed of • causes soil pore spaces to become smaller about 50 per cent solids (sand, silt, clay and organic • reduces water infiltration rate into soil matter) and about 50 per cent pore spaces. • decreases the rate that water will penetrate into the soil root zone and subsoil • increases the potential for surface Compaction concerns water ponding, water runoff, surface soil waterlogging and soil erosion Soil compaction can impair water Soil compaction infiltration into soil, crop emergence, • reduces the ability of a soil to hold root penetration and crop nutrient and can be a serious water and air, which are necessary for water uptake, all of which result in form of soil plant root growth and function depressed crop yield. • reduces crop emergence as a result of soil crusting Human-induced compaction of degradation. • impedes root growth and limits the agricultural soil can be the result of using volume of soil explored by roots tillage equipment during soil cultivation or result from the heavy weight of field equipment. • limits soil exploration by roots and Compacted soils can also be the result of natural soil- decreases the ability of crops to take up nutrients and forming processes. -
Drought and Ecosystem Carbon Cycling
Agricultural and Forest Meteorology 151 (2011) 765–773 Contents lists available at ScienceDirect Agricultural and Forest Meteorology journal homepage: www.elsevier.com/locate/agrformet Review Drought and ecosystem carbon cycling M.K. van der Molen a,b,∗, A.J. Dolman a, P. Ciais c, T. Eglin c, N. Gobron d, B.E. Law e, P. Meir f, W. Peters b, O.L. Phillips g, M. Reichstein h, T. Chen a, S.C. Dekker i, M. Doubková j, M.A. Friedl k, M. Jung h, B.J.J.M. van den Hurk l, R.A.M. de Jeu a, B. Kruijt m, T. Ohta n, K.T. Rebel i, S. Plummer o, S.I. Seneviratne p, S. Sitch g, A.J. Teuling p,r, G.R. van der Werf a, G. Wang a a Department of Hydrology and Geo-Environmental Sciences, Faculty of Earth and Life Sciences, VU-University Amsterdam, De Boelelaan 1085, 1081 HV Amsterdam, The Netherlands b Meteorology and Air Quality Group, Wageningen University and Research Centre, P.O. box 47, 6700 AA Wageningen, The Netherlands c LSCE CEA-CNRS-UVSQ, Orme des Merisiers, F-91191 Gif-sur-Yvette, France d Institute for Environment and Sustainability, EC Joint Research Centre, TP 272, 2749 via E. Fermi, I-21027 Ispra, VA, Italy e College of Forestry, Oregon State University, Corvallis, OR 97331-5752 USA f School of Geosciences, University of Edinburgh, EH8 9XP Edinburgh, UK g School of Geography, University of Leeds, Leeds LS2 9JT, UK h Max Planck Institute for Biogeochemistry, PO Box 100164, D-07701 Jena, Germany i Department of Environmental Sciences, Copernicus Institute of Sustainable Development, Utrecht University, PO Box 80115, 3508 TC Utrecht, The Netherlands j Institute of Photogrammetry and Remote Sensing, Vienna University of Technology, Gusshausstraße 27-29, 1040 Vienna, Austria k Geography and Environment, Boston University, 675 Commonwealth Avenue, Boston, MA 02215, USA l Department of Global Climate, Royal Netherlands Meteorological Institute, P.O. -
Dynamics of Carbon 14 in Soils: a Review C
Radioprotection, Suppl. 1, vol. 40 (2005) S465-S470 © EDP Sciences, 2005 DOI: 10.1051/radiopro:2005s1-068 Dynamics of Carbon 14 in soils: A review C. Tamponnet Institute of Radioprotection and Nuclear Safety, DEI/SECRE, CADARACHE, BP. 1, 13108 Saint-Paul-lez-Durance Cedex, France, e-mail: [email protected] Abstract. In terrestrial ecosystems, soil is the main interface between atmosphere, hydrosphere, lithosphere and biosphere. Its interactions with carbon cycle are primordial. Information about carbon 14 dynamics in soils is quite dispersed and an up-to-date status is therefore presented in this paper. Carbon 14 dynamics in soils are governed by physical processes (soil structure, soil aggregation, soil erosion) chemical processes (sequestration by soil components either mineral or organic), and soil biological processes (soil microbes, soil fauna, soil biochemistry). The relative importance of such processes varied remarkably among the various biomes (tropical forest, temperate forest, boreal forest, tropical savannah, temperate pastures, deserts, tundra, marshlands, agro ecosystems) encountered in the terrestrial ecosphere. Moreover, application for a simplified modelling of carbon 14 dynamics in soils is proposed. 1. INTRODUCTION The importance of carbon 14 of anthropic origin in the environment has been quite early a matter of concern for the authorities [1]. When the behaviour of carbon 14 in the environment is to be modelled, it is an absolute necessity to understand the biogeochemical cycles of carbon. One can distinguish indeed, a global cycle of carbon from different local cycles. As far as the biosphere is concerned, pedosphere is considered as a primordial exchange zone. Pedosphere, which will be named from now on as soils, is mainly located at the interface between atmosphere and lithosphere. -
Soil Carbon Science for Policy and Practice Soil-Based Initiatives to Mitigate Climate Change and Restore Soil Fertility Both Rely on Rebuilding Soil Organic Carbon
comment Soil carbon science for policy and practice Soil-based initiatives to mitigate climate change and restore soil fertility both rely on rebuilding soil organic carbon. Controversy about the role soils might play in climate change mitigation is, consequently, undermining actions to restore soils for improved agricultural and environmental outcomes. Mark A. Bradford, Chelsea J. Carey, Lesley Atwood, Deborah Bossio, Eli P. Fenichel, Sasha Gennet, Joseph Fargione, Jonathan R. B. Fisher, Emma Fuller, Daniel A. Kane, Johannes Lehmann, Emily E. Oldfeld, Elsa M. Ordway, Joseph Rudek, Jonathan Sanderman and Stephen A. Wood e argue there is scientific forestry, soil carbon losses via erosion and carbon, vary markedly within a field. Even consensus on the need to decomposition have generally exceeded within seemingly homogenous fields, a Wrebuild soil organic carbon formation rates of soil carbon from plant high spatial density of soil observations is (hereafter, ‘soil carbon’) for sustainable land inputs. Losses associated with these land therefore required to detect the incremental stewardship. Soil carbon concentrations and uses are substantive globally, with a mean ‘signal’ of management effects on soil carbon stocks have been reduced in agricultural estimate to 2-m depth of 133 Pg carbon8, from the local ‘noise’11. Given the time soils following long-term use of practices equivalent to ~63 ppm atmospheric CO2. and expense of acquiring a high density of such as intensive tillage and overgrazing. Losses vary spatially by type and duration observations, most current soil sampling is Adoption of practices such as cover crops of land use, as well as biophysical conditions too limited to reliably quantify management and silvopasture can protect and rebuild such as soil texture, mineralogy, plant effects at field scales9,10. -
The Nature and Dynamics of Soil Organic Matter: Plant Inputs, Microbial Transformations, and Organic Matter Stabilization
Soil Biology & Biochemistry 98 (2016) 109e126 Contents lists available at ScienceDirect Soil Biology & Biochemistry journal homepage: www.elsevier.com/locate/soilbio Review paper The nature and dynamics of soil organic matter: Plant inputs, microbial transformations, and organic matter stabilization Eldor A. Paul Natural Resource Ecology Laboratory and Department of Soil and Crop Sciences, Colorado State University, Fort Collins, CO 80523-1499, USA article info abstract Article history: This review covers historical perspectives, the role of plant inputs, and the nature and dynamics of soil Received 19 November 2015 organic matter (SOM), often known as humus. Information on turnover of organic matter components, Received in revised form the role of microbial products, and modeling of SOM, and tracer research should help us to anticipate 31 March 2016 what future research may answer today's challenges. Our globe's most important natural resource is best Accepted 1 April 2016 studied relative to its chemistry, dynamics, matrix interactions, and microbial transformations. Humus has similar, worldwide characteristics, but varies with abiotic controls, soil type, vegetation inputs and composition, and the soil biota. It contains carbohydrates, proteins, lipids, phenol-aromatics, protein- Keywords: Soil organic matter derived and cyclic nitrogenous compounds, and some still unknown compounds. Protection of trans- 13C formed plant residues and microbial products occurs through spatial inaccessibility-resource availability, 14C aggregation of mineral and organic constituents, and interactions with sesquioxides, cations, silts, and Plant residue decomposition clays. Tracers that became available in the mid-20th century made the study of SOM dynamics possible. Soil carbon dynamics Carbon dating identified resistant, often mineral-associated, materials to be thousands of years old, 13 Humus especially at depth in the profile. -
Agricultural Soil Carbon Credits: Making Sense of Protocols for Carbon Sequestration and Net Greenhouse Gas Removals
Agricultural Soil Carbon Credits: Making sense of protocols for carbon sequestration and net greenhouse gas removals NATURAL CLIMATE SOLUTIONS About this report This synthesis is for federal and state We contacted each carbon registry and policymakers looking to shape public marketplace to ensure that details investments in climate mitigation presented in this report and through agricultural soil carbon credits, accompanying appendix are accurate. protocol developers, project developers This report does not address carbon and aggregators, buyers of credits and accounting outside of published others interested in learning about the protocols meant to generate verified landscape of soil carbon and net carbon credits. greenhouse gas measurement, reporting While not a focus of the report, we and verification protocols. We use the remain concerned that any end-use of term MRV broadly to encompass the carbon credits as an offset, without range of quantification activities, robust local pollution regulations, will structural considerations and perpetuate the historic and ongoing requirements intended to ensure the negative impacts of carbon trading on integrity of quantified credits. disadvantaged communities and Black, This report is based on careful review Indigenous and other communities of and synthesis of publicly available soil color. Carbon markets have enormous organic carbon MRV protocols published potential to incentivize and reward by nonprofit carbon registries and by climate progress, but markets must be private carbon crediting marketplaces. paired with a strong regulatory backing. Acknowledgements This report was supported through a gift Conservation Cropping Protocol; Miguel to Environmental Defense Fund from the Taboada who provided feedback on the High Meadows Foundation for post- FAO GSOC protocol; Radhika Moolgavkar doctoral fellowships and through the at Nori; Robin Rather, Jim Blackburn, Bezos Earth Fund. -
Measuring Soil Carbon Change
Measuring soil carbon change Peter Donovan version: October 2013 This guide can be freely copied and adapted, with attribution, no commercial use, and derivative works similarly licensed. Contents What this guide is about, and how to use it iv 1 The work of the biosphere 1 1.1 Technology . 1 1.2 The carbon cycle . 2 1.3 Let, not make . 3 1.4 Monitoring: a strategic and creative choice . 4 2 Measuring soil carbon 7 2.1 Purpose, result, and uncertainty . 7 2.2 Change . 9 2.3 Organic and inorganic soil carbon . 11 2.4 Laboratory tests . 12 2.5 Getting started . 14 3 Site selection and sampling design 15 3.1 Mapping your site . 15 3.2 Stratification . 15 3.3 Locating plots . 17 3.4 Sampling tools . 17 3.5 Sampling intensity within the plot . 17 4 Sampling and field procedures 20 4.1 Lay out a transect and mark the plot center . 20 4.2 Soil surface observations . 23 4.3 Lay out the plot . 23 4.4 Use probe to take samples . 24 4.5 Soils with abundant rocks, gravel, or coarse fragments . 24 4.6 Characterize the soil . 25 4.7 Bag the sample . 26 4.8 Going deeper . 26 4.9 Sampling for bulk density . 27 4.10 Resampling . 29 4.11 Correcting for changes in bulk density . 29 ii 5 Getting your samples analyzed 31 5.1 Sample preparation . 31 5.2 Storing samples . 32 5.3 Split sampling to test your lab . 32 5.4 U.S. labs that do elemental analysis or dry combustion test .