Tag Archives: soil carbon storage

Applying equations to forests- carbon storage across environmental gradients in northeastern Puerto Rico

If you’ve ever read about carbon storage or sequestration (and if you’ve read my blog before, there’s a good chance you have), have you ever wondered how scientists come up with the numbers they love to throw around? How do we “know” that there are 684-724 petagrams of carbon to a depth of 30 cm in all the soils across the whole wide world? How could anyone possibly know that?

We don’t. And we can’t. But there are those crazy enough to try, and trying essentially boils down to  sampling, sampling, sampling, then a whole lot of extrapolating. If you imagine a landscape in which there is a continuous but highly variable distribution of carbon, the only way we’re gong to get any sort of meaningful estimate of the total is to dig a lot of holes. The points you see below represent a lot of holes that I actually helped dig! (I’m one of those crazies). I’ve thrown them up over this topographical surface to give you a sense of just how variable carbon can be across space.

Rather than subject you to a discussion of a ecosystem carbon storage, I’d like to share some pretty pictures I’ve been putting together. I’m attempting to create a model for carbon storage across a roughly 10 km area of forest in northeastern Puerto Rico that is underlain by two bedrock types, contains three distinct forests dominated by different tree species, and has broad gradients in temperature and rainfall across the topographically varied landscape.

Bluer regions represent areas of greater carbon storage while yellower regions store less carbon. Essentially I’ve created an image made of a series of pixels -here, the resolution is coarse enough that you can distinguish individual pixels around the edges. For each pixel, a predicted carbon value has been calculated from a very simple equation that takes bedrock, forest type and elevation into account.

Breaking it down by forest type…



That’s all for now, hopefully I’ll have more and more interesting pictures to show in the future.

Carbon sequestration in soils: sources, sinks and pitfalls

When we talk about “sequestering” carbon in the soil to mitigate anthropogenic climate change, what are we really saying as scientists, and what is the public getting from it?  And perhaps even more importantly, what implicit assumptions are we as scientists making that may affect the validity of the widely held belief that increased C storage in soils is a good thing, and can offset our CO2 emissions?

In a recent soil carbon series in the European Journal of Soil Science, one review paper attempts to address these issues. “Carbon sequestration” has become a popular idea among policy makers and scientists alike. As anyone who keeps up on ecosystem science literature will know, C sequestration has also become an explicit motivation for numerous studies of soil and ecosystem properties.

Current best estimates claim that worldwide, soils store 684-720 Pg of C within the upper 30 cm, and 1462-1548 Pg to a depth of 1m. (For anyone not familiar with these terms, 1Pg = 1×10ˆ15 gram). The upper 30% of the soil profile to 1m clearly stores a disproportionate amount of C; this ecologists know to be the zone where continuous inputs from roots and organic matter replenish C. To put these numbers in an ecosystem context, the amount of C stored globally in soils to 30cm is twice the amount  of C stored as CO2 in the atmosphere and three times the amount of C stored in above ground vegetation. Clearly, soils represent a huge pool in global C budgets and should be managed with the knowledge that changes may represent a powerful feedback on the global C cycle. This vast storage potential is what has popularized the idea of sequestering even more C in soils and has spurred a myriad of different research approaches, from ecosystem-scale reforestation efforts to molecular studies of C-mineral binding interactions.

Given the amount of hope that has already been invested in this powerful idea, it is important for scientists interested in soil C to keep several caveats in mind when planning and conducting their research, and when communicating that research to a broader audience at a science or policy conference.

Caveat #1) Carbon sequestration does not necessarily mean climate change mitigation.

Increasing the amount of C stored in a particular ecosystem’s soil does not by default decrease the amount of CO2 released to the atmosphere. This is partially an issue of scale. If policy makers choose to set aside a certain amount of pasture land for reforestation (with the assumption that this will increase the net C storage in these systems), it is often the case that new land will have to be cleared somewhere else to compensate for the lost agricultural production.  The clearest way around this problem is to be selective in land use changes: land that is more fertile should be exploited for farming, and land that is less fertile should be reforested to boost C storage. However, an increasing global population poses obvious constraints to this line of reasoning. Ultimately, the fact remains that in the upcoming decades, we will need to boost our agricultural yields to meet global demand, and furthermore, climate change is predicted to decrease the fertility of some of the world’s most productive regions.

Moreover, allowing land to go back to its “natural” state does not necessarily lead to a net accumulation of C. A forest respires far more CO2 per acre than a wheat field. Due to the high water demands of forests relative to crops, it can sometimes be the case that trees dry up otherwise inundated subsurface soils, and in doing so create a soil environment that accelerates the decomposition of C.  One must have a refined understanding of the sources and sinks of CO2 in any particular ecosystem to claim that it will or will not “sequester” C.

Finally, management changes leading to increased C storage may increase or decrease the flux of other greenhouse gases, most notably N2O and methane. Given that these gases have 298 and 25 times the global warming potential of CO2, respectively, they are not a trivial consideration. Forests often hold less nitrogen than pastures (due to the different C:N demands of woody vs. non-woody tissue), and consequently release more N2O through the microbial process known as denitrification.

Caveat #2) The amount of carbon that can be locked up in soil in finite

Our understanding of how C is actually “stabilized” in soil on a molecular scale is still evolving. Scientists are using powerful technologies such as x-ray crystallography to understand in detail the chemical interactions between soil minerals and carbon-rich compounds that cause C to be tightly bound and inaccessible to microbes. As a general rule, the more mineral surface area available for C binding, the more tightly C is bound. In subsurface soils lower levels of C mean higher (mineral surface area: C) ratios and thus tighter binding of the C that is present.

However, mineral stabilization has its limits. Laboratory experiments are finding that as C is added to soils, “steady states” are sequentially reached. Careful manipulation of the  chemical and thermodynamic parameters of a soil may bump that soil from a lower steady state to a higher one, but whether such techniques can be applied on a whole-ecosystem scale remains to be seen.

To repeat, caveat #2 is that the amount of carbon that can be locked up in soil is finite, which leads to caveat #3.
At present, the amount of CO2 we put in the atmosphere does not seem to be.

Powlson et al. 2011. Soil carbon sequestration to mitigate climate change: a critical re-examination to identify the true and the false. European Journal of Soil Science 62: 42-55.

Earthworms play key role in regulating carbon storage in tropical ecosystems

A principle frontier in our understanding of global carbon budgets is tropical forests, on which research is historically scarce. At temperate and high latitudes, a warmer climate is predicted to increase the rate of decomposition and soil carbon turnover, resulting in a positive feedback on atmospheric carbon as CO2 is released from soils at increasing rates. A better understanding of the mechanisms regulating tropical carbon storage is needed in order to develop a holistic picture of global carbon cycling and feedbacks due to climate change.

Earthworms are important regulators of many ecological properties of soils. Their burrowing activity increases soil pore space and contributes to soil structure and drainage. Most importantly, earthworms can digest a huge quantity of dead and partially decomposed plant material. This digestion causes chemical transformations that ultimately produce nutrient-rich soil organic matter, or SOM. SOM helps ensure soil fertility, and contributes to numerous physical and chemical soil properties such as soil structure, porosity, water retention, and the capacity of soils to buffer pH changes. SOM’s aggregate structure causes it to have high water stability. This is an essential property in tropical forests, which have the highest rainfall levels of any biome on Earth.

SOM produced by earthworms is also rich in both carbon and nitrogen. A detailed biochemical and molecular analysis of earthworm casts suggests that these creatures may in fact play a key role in controlling tropical carbon storage.

Casts are clumps of digested organic matter excreted by earthworms that aggregate into large and distinctive structures. Researchers working in the rain forest neighboring the Dong Cao village in Northeast Vietnam studied the effect of cast production by Amynthas Khami on soil C storge. A. Khami is a species of tropical earthworm that can grow up to 50 cm long and produce tower-like casts. The researchers first used a “simulated rainfall” experiment to determine the relative stability of casts versus control soils. They then measured total carbon content, lignin and mineral-bound SOM content of casts and control soils.

An earthworm cast produced by A. Khami, a large tropical species found in Northeast Vietnam.

The study found striking differences in the chemical composition of earthworm casts versus control soils that ubiquitously indicate higher carbon storage in casts. Casts are more structurally stable and can withstand at least twice as long a rainfall event as control soils without compromising their structural integrity. They are enriched in carbon compared with controls, and particularly in carbon compounds such as lignin that have a high “carbon storage” potential. Lignin, a primary constituent of woody plant tissue, is a complex and heterogeneous molecule that is both carbon-rich and difficult for microbes to decompose. Earthworms probably excrete high quantities of lignin after obtaining the more digestible carbon sources from the roots and leaves that they eat. Finally, high levels of mineral associated-SOM were found in casts. Soil minerals bind to organic matter through electrostatic interactions, and in doing so make it unavailable for decomposers.

Though it well known that earthworm digestion initially speeds up decomposition, this new study suggests that casts may in fact contribute to long-term carbon stabilization. In tropical soils, which tend to cycle carbon quite rapidly, this mechanism should not go unappreciated. Future tropical land-use decisions may want to account for the welfare of this often-unappreciated soil organism.

Hong et al. 2011. How do earthworms influence organic matter quantity and quality in tropical soils? Soil Biology and Biochemistry 43: 223-230.