Monday, December 14, 2015

COP21 and "4 per thousand" - Storing Carbon in the Soil.

It would have been a remarkable oversight, had not our use of the land and its soils featured among the discussions about climate change mitigation in Paris at COP21. However, at the conference was hosted a side-event and official launch of the "4 per thousand" initiative, which aims to increase soil carbon over a 25 year period, with the effect of halting the annual increase in CO2 in the atmosphere. It is important to be aware of what "4/1000" means: it is not an increase in the overall soil carbon by an annual 4 grams per 1000 grams of soil as has been claimed, but an increase in the existing carbon in the topsoil by 0.4%/year. This has been described from an Australian perspective:

"Let us start with the analogy of a football field (Soccer, not rugby!). Imagine it is a fifth larger than normal – making it one hectare in size. The top layer of soil on the field, 30 cm deep, is known as the topsoil.

"Carbon is the main ingredient of organic matter, so organic matter is often referred to as ‘soil organic carbon’. In Australian soils, this organic matter makes up on average, between 1 and 3 percent of the topsoil. For the purpose of the exercise, we will assume that the topsoil on the football field contains 1.5 percent carbon. This equates to 58 tonnes of carbon in the topsoil across the whole football field.What the French Government is calling for is to increase that 58 tonnes by 0.4 percent per annum – in our imaginary football field that would equate to an increase of 0.2 tonnes (or 200 kg) of carbon in the topsoil each year."

Thus, the annual carbon increase is 0.4% of 1.5%, or 0.006%, giving a total soil carbon content of 1.506% after year 1, and 1.65% after 25 years, with around 6 tonnes of carbon having been captured per hectare. Done on the global scale, the impact could be enormous. The “4/1000 Initiative: Soils for Food Security and Climate” aims to integrate agriculture as part of the climate change solution, rather than being the major problem it is often deemed to be, which along with forestry and other land-use, contributes 24% of global greenhouse gas emissions. The total amount of carbon stored in soils is reckoned at 2,400 billion tonnes, making it the largest terrestrial carbon pool. The total carbon emissions by humans amounts to an annual 8.9 billion tonnes, and so the ratio 8.9/2,400 = 0.4%, which is where the "4/1000" figure comes from.

However, it is the annual rate of carbon sequestration per hectare which is the critical determinant of how successful the strategy is likely to be. As has been noted:

"The land area of the world has 149 million km2, and it would be estimated that on average there are 161 tonnes of C per hectare. So 0.4% of this equates to an average sequestration rate to offset emissions at 0.6 tonnes of C per hectare per year. We know that soil varies widely in terms of C storage, for example peat soils in the tropics hold about 4000 tonnes of C per hectare, while sandy soils in arid regions may only hold 80 tonnes of C. The type of above ground vegetation and how quickly the soil biota uses the carbon also can affect this rate. Taking this into account, we would need to add about 4 times the amount of organic matter to meet this sequestration rate."

Previous studies have concluded that a global mean storage rate of 0.5 tonnes of carbon/hectare/year is possible, and research from the Rodale Institute concluded that if their regenerative practices were carried out across the world's agricultural lands, it would be possible to capture all human carbon emissions. Thus, while achieving a global "4/1000" poses an appreciable challenge, even approaching this target would be of considerable benefit, not only in terms of helping to balance the global carbon books, but in improving and restoring the quality of the world' soils. The world's cultivated soils are estimated have lost between 50 and 70% of their original carbon content, a trend that can be reversed by using defined agricultural methods. The result is more productive, carbon-rich soils, and so the strategy is able to “reconcile food security and climate change.”


The essential methods for 4/1000:
  • Avoid leaving the soil bare in order to limit carbon losses
  • Restore degraded crops, grasslands and forests
  • Plant trees and legumes which fix atmospheric nitrogen in the soil
  • Feed the soil with manure and composts
  • Conserve and collect water at the feet of plants to favour plant growth
If good practices and introduced and sustained, it is expected that the carbon capture will continue for 20 to 30 years.

Applied to the surface horizon of the world's soils, which contain 860 billion tonnes of carbon, the 4‰ target would result in 3.4 billion tonnes carbon being stored annually, which amounts to around 40% of anthropogenic CO2 emissions. The majority of soils, not only agricultural soils, could be so addressed, including forests. The above practices could be undertaken by almost half the world's population, those living in rural areas, working 570 million mostly small farms.

The likely costs?

For crops, $20 to $40 (US) per tonne of CO2. For grasslands and forests, $50 or $80 (US) per tonne of CO2.

Tuesday, December 08, 2015

Phytoremediation - Using Plants to Cleanse the Earth.

Phytoremediation1,2 may be defined as the treatment of environmental problems by using plants in situ to avoid the need to excavate the contaminated material for disposal elsewhere. It can be applied to the amelioration of contaminated soils, water, or air, using plants that can contain, degrade, or eliminate metals, pesticides, solvents, explosives, crude oil and its derivatives (refined fuels), and related contaminating materials. Phytoremediation has been used successfully for the restoration of abandoned metal-mine workings, and cleaning up sites where polychlorinated biphenyls have been dumped during manufacture, and for the mitigation of on-going coal mine discharges. Phytoremediation uses the natural ability of particular plants (“hyperaccumulators”, described below) to bioaccumulate, degrade, or otherwise reduce the environmental impact of contaminants in soils, water, or air. Those contaminants that have been successfully mitigated in phytoremediation projects worldwide are metals, pesticides, solvents, explosives, and crude oil and its derivatives, and the technology has become increasingly popular and has been employed at sites with soils contaminated with lead, uranium, and arsenic. A major disadvantage of phytoremediation is that it takes a relatively long time to achieve, because the process rests upon the ability of a plant to thrive in an environment that is not normally ideal for plants.

Advantages and limitations of phytoremediation.
  • Advantages:
    • The cost of phytoremediation are lower than those of traditional processes, both in situ and ex situ.
    • The plants can be easily monitored.
    • There is the possibility of the recovery and re-use of valuable metals (by companies specializing in “phyto-mining”).
    • It is potentially the least harmful method because it uses naturally occurring organisms and preserves the environment in a more natural state.
    • Trees may be used in phytoremediation, since they grow on land of marginal quality, have long life-spans and a high flood tolerance. Willows and poplars are most commonly used, and can grow 6-8 feet (ca 2 metres) per year. For deep contamination, hybrid poplars with roots extending 30 feet deep have been used, which penetrate microscopically sized pores in the soil matrix and each tree can cycle 100 L of water per day, functioning almost as a solar powered and self-contained pump and treatment system.
    • Phytoscreening is possible, in which plants may be used as biosensors for particular types of contaminants, thus giving a signal of underlying contaminant plumes, e.g. trichloroethene has been detected in the trunks of trees.
    • Genetic engineering may confer improvements to phytoremediation, e.g. genes encoding a nitroreductase from a bacterium, when inserted into tobacco, increased the resistance of the plant to the toxic effects of TNT and the uptake of the material. Plants may be genetically modified to grow in soils even when the pollution levels in the soil are lethal for non-treated plants, and to absorb a greater concentration of the contaminant.
  • Limitations:
    • Phytoremediation is limited to the surface area and depth occupied by the plant roots.
    • Slow growth and low biomass require a long-term commitment.
    • Using plants, it is not possible to prevent entirely the leaching of contaminants into the groundwater (without the complete removal of the contaminated ground, which in itself does not resolve the problem of contamination).
    • The survival of the plants is affected by the toxicity of the contaminated land and the general condition of the soil.
    • Bio-accumulation of contaminants, especially metals, into plants which then pass into the food chain, from primary level consumers upwards, or that the safe disposal of the affected plant material is required, i.e. if the plants might be eaten by animals.
    • The procedure is slow.
Hyperaccumulators and biotic interactions. 
If a plant is able to concentrate a particular contaminant, to a given minimum concentration (> 1000 mg/kg of dry weight for nickel, copper, cobalt, chromium or lead; or > 10,000 mg/kg for zinc or manganese), it is categorized as a hyperaccumulator. This capacity for accumulation is a result of genetic adaptation over many generations in hostile environments. Metal hyperaccumulation can affect various different factors, such as protection, interferences between different species of plants, mutualism (e.g. mycorrhizae, pollen and seed dispersal), commensalism, and biofilm.

Different possible phytoremediation methods.
Various processes that are mediated by plants or algae might be used to address environmental problems:
  • Phytoextraction — uptake and concentration of substances from the environment into the plant biomass.
  • Phytostabilization — reducing the mobility of substances in the environment, for example, by limiting the leaching of substances from the soil.
  • Phytotransformation — chemical modification of environmental substances as a direct result of plant metabolism, often resulting in their inactivation, degradation (phytodegradation), or immobilization (phytostabilization).
  • Phytostimulation — enhancement of soil microbial activity for the degradation of contaminants, typically by organisms that associate with roots. This process is also known as rhizosphere degradation. Phytostimulation can also involve aquatic plants supporting active populations of microbial degraders, as in the stimulation of atrazine degradation by hornwort.
  • Phytovolatilization — removal of substances from soil or water with release into the air, sometimes as a result of phytotransformation to more volatile and/or less polluting substances.
  • Rhizofiltration — filtering water through a mass of roots to remove toxic substances or excess nutrients. The pollutants remain absorbed in or adsorbed to the roots. 
Phytoextraction.
In phytoextraction (or phytoaccumulation) plants or algae are used to extract contaminants from soils, sediments or water into harvestable plant biomass (those organisms that take larger-than-normal amounts of contaminants from the soil are called hyperaccumulators). Phytoextraction has been used more often for extracting heavy metals than for organic contaminants. The plants absorb contaminants through the root system which they then contain in the root biomass and/or move them into the stems and/or leaves. A living plant may continue to absorb contaminants until it is harvested. After harvest, a lower level of the contaminant will remain in the soil, so the growth/harvest cycle must usually be repeated through several crops to achieve a significant cleanup. The process can be repeated to affect further decontamination. There are two forms of phytoextraction:
  • Natural hyper-accumulation, where plants take up the contaminants in soil unassisted.
  • Induced (assisted) hyper-accumulation, in which a conditioning fluid containing a chelator or another agent is added to soil to increase metal solubility or mobilization so that the plants can absorb them more easily. In many cases natural hyperaccumulators are metallophyte plants that can tolerate and incorporate high levels of toxic metals.

Examples of phytoextraction:
  • Arsenic, using the Sunflower (Helianthus annuus), or the Chinese Brake fern (Pteris vittata), a hyperaccumulator. Chinese Brake fern stores arsenic in its leaves.
  • Cadmium, using willow (Salix viminalis): willow has a significant potential as a phytoextractor of cadmium (Cd), zinc (Zn), and copper (Cu), as willow has some specific characteristics like high transport capacity of heavy metals from root to shoot and huge amount of biomass production; can be used also for production of bioenergy in the biomass energy power plant.
  • Cadmium and zinc, using Alpine pennycress (Thlaspi caerulescens), a hyperaccumulator of these metals at levels that would be toxic to many plants, although its growth appears to be inhibited by copper.
Phytostabilization.
In phytostabilization the intention is to stabilize, or contain the pollutant over the long-term. There may be a number of contributing factors to this, e.g. the reduction of wind (soil) erosion by the body of the plant, but the roots of the plant can resist water (soil) erosion, immobilize the pollutants by adsorption or accumulation, and provide a zone around the roots where the pollutant can be deposited in an immobilized form. In contrast with phytoextraction, phytostabilization aims mainly to sequester pollutants in soil around the roots but not in the plant tissues. Hence the pollutants are increasingly less bioavailable, such that exposure to livestock, wildlife, and humans is reduced. Mine tailings may be stabilized by growing a vegetative cap.


Phytotransformation. 
 Some plants, e.g. cannas, are able to detoxify organic pollutants - pesticides, explosives, solvents, industrial chemicals, and other xenobiotic substances  - by metabolising them. The metabolic functions of microorganisms living in association with plant roots may also metabolize these substances, as present in soil or water. Due to the complex and recalcitrant nature of many of these compounds, they cannot be broken down entirely (mineralised) to basic molecules (H2O, CO2, etc.) by plants and hence the term phytotransformation represents molecular alterations rather than the complete decomposition of the compound. Phytotransformation may be viewed1 as a "Green Liver" because plants behave analogously to the human liver in processing these xenobiotic compounds, introducing polar groups such as –OH to them. This is known as Phase I metabolism, similar to the way that the human liver increases the polarity of drugs and foreign compounds. In plants, it is enzymes such as nitroreductases which carry out these transformations, whereas in the human liver it is enzymes such as the Cytochrome P450s that perform the task. Phase II metabolism in the second step in phytotransformation, in which the polarity of the xenobiotic molecule is increased by combination with plant biomolecules such as glucose and amino-acids. This is called “conjugation”, and is once more similar to processes such as glucoronidation (addition of glucose) and glutathione addition reactions, catalysed by appropriate enzymes. The effect of the two metabolic steps may serve to detoxify the xenobiotic and aid its mobilization via aqueous channels. In Phase III metabolism, the xenobiotic becomes sequestered, by incorporation in a complex “lignin-type” structure, where it is kept apart from the normal functioning of the plant. The phytotransformation of trinitrotoluene (TNT) has been well studied, and a detailed mechanism proposed for it.

Phytostimulation and rhizoremediation. 
This term identifies the process where compounds released from plant roots enhance microbial activity in the rhizosphere, which is the narrow region of soil around the roots of plants, and associated soil microorganisms. Soil which is not part of the rhizosphere is known as bulk soil. In rhizoremediation, microorganisms degrade soil contaminants in the rhizosphere. It is usual that those soil pollutants which are remediated by this method are highly hydrophobic xenobiotics, and are hence unable to enter the plant. Rather than the plant being a main protagonist in this process, it creates a haven in which microorganisms in the rhizosphere are able to perform the degradation.The plant acts as a solar-powered pump, which draws in both water and the xenobiotic agent, simultaneously producing substrates (e.g. root exudates and root turnover) that assist the growth of the microbes which act as pollutant degrading agents. Microbial activity is stimulated in the rhizosphere through a number of different routes: (i) exudates, e.g. sugars, carbohydrates, amino acids, acetates, and enzymes, nourish indigenous microbe populations; (ii) root systems bring oxygen into the rhizosphere, meaning that aerobic transformations are supported; (3) the available organic carbon is enhanced through the growth of fine-root biomass; (4) mycorrhizae fungi, which are an essential component of the rhizosphere, provide unique enzymatic pathways lending the capacity to degrade pollutant molecules that would not be degraded by bacteria alone; and (5) the presence of plants (and their roots) creates a domain for microbial populations, which are activated in the rhizosphere. There have been five enzyme systems identified in soils: (i) dehalogenase (which acts in dechlorination reactions of chlorinated hydrocarbons); (ii) nitroreductase (essential for the initial step of nitroaromatic degradation); (iii) peroxidase (a critical catalyst for oxidation reactions); (iv) laccase (able to begin the decomposition of otherwise robust aromatic ring structures); (v) nitrilase (another key factor in oxidation processes). The method is limited in that when there are high concentrations of pollutants present, the plants may be overwhelmed and die. The successful use of phytostimulation has been demonstrated in the remediation of chlorinated solvents from groundwater, petroleum hydrocarbons from soil and groundwater and PAHs from soil. 

Phytovolatilization.
Probably, this is the most controversial of the phytoremediation technologies, since it involves the release of contaminants either directly, or in a metabolically modified form, into the atmosphere. Phytovolatilization3 has been used principally for the removal of Hg2+ ions which are transformed into less toxic elemental mercury4. Tritium (3H), a radioactive isotope of hydrogen with a half-life of about 12 years, decaying to helium, has also been removed by phytovolatilization5. A good deal more research is necessary before this strategy becomes mainstream, since there are various negative features to be addressed. For example, mercury that is released into the atmosphere from plants is likely to be recycled by precipitation and thus returned the ecosystem, and the method is restricted both to sites where the concentration of contaminants is toward the low side, and where the contamination is no deeper than the roots of the plants being used. 

Rhizofiltration. 
Rhizofiltration6 involves filtering contaminated water through a mass of roots for the extraction of contaminants, or excess nutrients, e.g. phosphorus. The contaminated water can either be collected from a waste site and taken to where plants are being hydroponically cultivated, or the plants may be planted in the area directly. In both cases, the roots draw up the water and its associated contaminants. This process is very similar to phytoextraction in that the contaminants become sequestered in the form of harvestable plant biomass. Then new plants are grown and harvested until a satisfactory degree of decontamination is achieved. It is the concentration and precipitation of heavy metals that is sought principally. While noting these similarities, the fundamental difference between the two approaches is that rhizofiltration is used in aquatic environments, while phytoextraction is applied to the decontamination of soils. There are limitations to rhizofiltration. As usual in phytoremediation methods, any contaminant that is below the rooting depth will not be extracted, and if the level of contamination is too high the plants will not grow. Depending on the type of plant and contaminant, the process may need to be continued over a protracted period, before regulatory levels are achieved. It is generally true that many different kinds of contaminants will be present – in some cases a mixture of organics and heavy metals – and thus the use of rhizofiltration alone is unlikely to succeed. Importantly, the plants chosen should be non-fodder crop to minimize poisoning animals, which might eat them in contaminated form.  That noted, the effective removal of heavy metal cations, e.g. Cu2+, Cd2+, Cr6+, Ni2+, Pb2+, and Zn2+ from aqueous solutions has been demonstrated7, and the removal of low-level radionuclides, from liquid streams8. In that latter application, a “feeder layer” of soil is suspended above the stream through which plants grow, from which the plant roots extend downward into the water. In this way, fertilizer can be used to help the plants to grow, while avoiding adding to the contamination of the stream, while the latter is cleansed of heavy metal cations9. Rhizofiltration is cost-effective when large volumes of water must be treated containing low concentrations of contaminants. Inclusive of the costs of the capital outlay and final waste disposal, the cost of removing radionuclides from water using sunflowers was reckoned (at 1996 prices) at $2─6 per thousand gallons of water treated10.
 


References. 
(1) Burken, J.G. (2004), "2. Uptake and Metabolism of Organic Compounds: Green-Liver Model", in McCutcheon, S.C.; Schnoor, J.L. (Eds.), Phytoremediation: Transformation and Control of Contaminants, A Wiley-Interscience Series of Texts and Monographs, Hoboken, NJ: John Wiley, p. 59, doi:10.1002/047127304X.ch2, ISBN 0-471-39435-1.
(2) http://en.wikipedia.org/wiki/Phytoremediation.
(3) http://www.unep.or.jp/Ietc/Publications/Freshwater/FMS2/2.asp.
(4) http://tede.ibict.br/tde_busca/arquivo.php?codArquivo=431.
(5) Dushenkov, S. (2003) “Trends in phytoremediation or radionuclides.” Plant and Soil, 249, 167. (6) http://en.wikipedia.org/wiki/Rhizofiltration.
(7) EPA, (1998) “A Citizen's Guide to Phytoremediation,.” U.S. Environmental Protection Agency, Office of Solid Waste and Emergency Response,” EPA 542-F-98-011, August. 
(8) Dushenkov, V., Motto, H., Raskin, I. and Nanda Kumar, P.B.A. (1995) "Rhizofiltration: the Use of Plants to Remove Heavy Metals From Aqueous Streams." Environmental Science Technology 30, 1239. 
(9) Raskin, I., Smith, R.D. and Salt, D.E. (1997) "Phytoremediation of Metals: Using Plants to Remove Pollutants from the Environment." Current Opinion in Biotechnology. 8, 221. 
(10) Cooney, C. M. (1996) "Sunflowers Remove Radionuclides From Water in Ongoing Phytoremediation Field Tests." Environmental Science and Technology 30, 194.