List, Crispin, Paul 

I saw the stove list introduction of today's "downstream" thread after writing 
the following which started on the "geo list yesterday. 

To Paul (message on this topic not shown below), I would say that you are 
addressing a real problem for disappearance of char (floating away) - but that 
this article is talking only about dissolved black carbon (DBC) 

To Crispin (message on this topic not shown below either), I will write a 
separate response - pointing out how little our friend Watts understands of 
these topics - and that you should be looking for other authorities on future 
global temperatures. 

I will also send this below right away (as I had planned) to the 
"biochar-policy" and "biochar-soil" lists 

Ron 

----- Original Message -----
From: [email protected] 
To: [email protected] 
Cc: [email protected] 
Sent: Saturday, April 20, 2013 6:39:40 PM 
Subject: Re: [geo] RE: Biochar: Downstream effects 



Greg and list: 

I have tried to figure out whether this paper by Jaffe et al is apt to harm or 
help the introduction of biochar. My perception is that Jaffe and co-authors 
see a fairly strong connection to biochar, but I am not so sure. There is so 
little biochar in place that what was being measured was almost entirely from 
forest fires, which char can be very different from what is now being tested . 

The persons at NSF who wrote up the press release (below) certainly tied this 
article in to biochar development. For those who don't subscribe to Science, 
here is what Jaffe etal said about biochar - 4 sentences in the last part of 
the last paragraph (with my comments on each in bold): 

"1. Bio-char applications to soils have been proposed as an effective means of 
carbon sequestration (30). 
RWL1: Certainly true and non controversial. (30) is J. Lehmann, J. Gaunt, M. 
Rondon, Mitig. Adapt. Strat. Gl. 11, 403 (2006) and is a good early background 
reference (at a time before biochar received its present name) . 

2. This activity may further enhance the translocation and export of DBC to 
marine systems. 
[RWL2: Also true - but equally true could be "may not". The key is whether the 
material now ending up as DBC is more apt to be used by microbes and fungus - 
ending up mostly as CO2. Biochar literature says almost nothing about DBC, 
except that it is small. Char is presently used to absorb (not release) the 
polyaromatic compounds that I gather are being measured to compute DBC. 

3. The environmental consequences of this are presently unknown but may be 
reflected in the reduction of DOC bioavailability and associated effects on 
microbial loop dynamics and aquatic food webs. 
[RWL3: Again, I think the key word is "may " . Biochar is being promoted to 
increase terrestrial biomass. In the Amazon, terra preta soils have double and 
triple the soil productivity - so maybe there will be also increased DOC 
bioavailability. It also seems likely that a world with much biochar will have 
fewer and smaller forest fires. Also char, being placed deep in soils, will 
generally not be found as much in surface runoff as will char from forest 
fires. 

4. Our data suggest that we apply our existing knowledge on DOC production, 
storage, and movement in soils to ensure that biochar applications are 
implemented sustainably and managed in ways to minimize riverine DBC fluxes. " 
[RWL4: This is a welcome offer to help investigate the biochar connection 
further. But I felt that DOC was being welcomed for ocean health reasons, and 
so if DOC and DBC are closely coupled, maybe there is a way for biochar to 
optimize both. Biochar is getting cre dit for preventing the release of excess 
fertilizers that are certainly harming ocean health, as well as wasting scarce 
farm-owner funds. Biochar's optimum temperature may be tunable to help in this 
tradeoff, if further research shows there is need for one. 

Part B 
Science magazine also has an introductory piece (p 287-288 ) in this same 
issue, by Rice University Prof. Caroline Massielo. Besides authoring five of 
the Jaffe etal cites, Dr. Masiello heads a biochar department at Rice and has 
authored numerous biochar papers. In her final four-sentence paragraph she says 
about the connection to biochar: 

5. "Jaffé et al. mention that biochar soil amendment may have unintended 
consequences through increased transport of DBC into aquatic and marine 
systems, with downstream impacts on aquatic food webs." 
[RWL5. It is not clear to me whether she is referencing positive or negative 
consequences/impacts. I am pretty sure that in most soils, the char is 
retaining, not releasing, dissolved carbon compounds. 

6. "These possibilities must be taken seriously." 
[RWL6: So perhaps the possibilities are mostly seen as negative - mostly 
thinking I guess of carcinogenic PAH compounds 

7. "The successful scaling-up of biochar soil amendment will require assessment 
of the fate of biochar carbon both in the solid and dissolved phases. 
[RWL7: Dr. Masiello is raising the additional topic of biochar proponents 
wanting long biochar lifetime - both solid and dissolved. Jaffe etal say in 
their first paragraph that charcoal ".... is ubiquitous in the environment, 
where it slowly decomposes, but part of it is preserved for thousands of years 
." This long lifetime (clouded by the term " part of" ) is rarely acknowledged 
by biochar's (very few) critics. 

8. Jaffé et al.’s observation that the aromatic, dissolved fraction of BC 
behaves at least in part like bulk DOC may make tracking DBC that much easier. 
(Emphasis added) 
[RWL8: I think this similarity globally between BOC and BDC is the key new 
conclusion of the Jaffe paper and the Masiello introductory perspective. But we 
still have the word "may" re tracking. Presumably it will be many years before 
there is sufficient riverine DOC and DBC from biochar to even be detected. 
Perhaps insightful lab tests can be conducted sooner. 

[RWL9: My prior reading in this area says that biochar users are apt to lean 
towards lower temperature chars, where there is little production of PAH's - 
the clearly undesirable part of DBC. Neither paper is explicit on this PAH 
topic. 

So in sum, I remain confused as to what to expect for both a) future DBC 
release from biochar and b) the resultant DBC impacts - in rivers or the ocean. 
I would welcome other input on the significance of the Jaffe etal paper. I do 
not now think it raises any new hurdles for large-scale biochar introduction. 

RWL10 - see below 

Ron 

----- Original Message -----
From: "Greg Rau" <[email protected]> 
To: [email protected] 
Sent: Friday, April 19, 2013 11:42:13 AM 
Subject: [geo] RE: Biochar: Downstream effects 

Here's the Science link: 
http://www.sciencemag.org/content/340/6130/345.abstract 

________________________________________ 
From: [email protected] [[email protected]] on 
behalf of Rau, Greg [[email protected]] 
Sent: Thursday, April 18, 2013 10:56 PM 
To: [email protected] 
Subject: [geo] Biochar: Downstream effects 

Press Release 13-069 
Where Does Charcoal, or Black Carbon, in Soils Go? 


Scientists find surprising new answers in wetlands such as the Everglades 
[Charred boreal forest after a fire] 

Charred boreal forest after a fire has raged: where does the "charcoal" go? 
Credit and Larger 
Version<http://www.nsf.gov/news/news_images.jsp?cntn_id=127577&org=NSF> 


April 18, 2013 

Scientists have uncovered one of nature's long-kept secrets--the true fate of 
charcoal in the world's soils. 

The ability to determine the fate of charcoal is critical to knowledge of the 
global carbon budget, which in turn can help understand and mitigate climate 
change. 

However, until now, researchers only had scientific guesses about what happens 
to charcoal once it's incorporated into soil. They believed it stayed there. 

Surprisingly, most of these researchers were wrong. 

The findings of a new study that examines the result of charcoal once it is 
deposited into the soil are outlined in a paper published this week in the 
journal Science. 

The international team of researchers was led by scientists Rudolf Jaffe of 
Florida International University and Thorsten Dittmar of the German Max Planck 
Society. 

"Most scientists thought charcoal was resistant," says Jaffe. "They believed 
that once it was incorporated into soils, it stayed there. But if that were the 
case, soils would be black." 

Charcoal, or black carbon, is a residue generated by combustion including 
wildfires and the burning of fossil fuels. 

When charcoal forms, it is usually deposited into the soil. 

"From a chemical perspective, no one really thought it dissolved, but it does," 
Jaffe says. 

"It doesn't accumulate for a long time. It's exported into wetlands and rivers, 
eventually making its way to the oceans." 

It all started with a strange finding in the Everglades. 

At the National Science Foundation (NSF) Florida Coastal Everglades Long-Term 
Ecological Research (LTER) site--one of 26 such NSF LTER sites in ecosystems 
around the 
world<http://www.nsf.gov/cgi-bin/goodbye?http://www.lternet.edu/sites/map>--Jaffe
 studied the glades' environmental chemistry. 

Dissolved organic carbon is known to be abundant in wetlands such as the 
Everglades and plays a critical role in the ecology of these systems. 

Jaffe wanted to learn more about what comprised the organic carbon in the 
Everglades. 

He and colleagues discovered that as much as 20 percent of the total dissolved 
organic carbon in the Everglades is charcoal. 

Surprised by the finding, the researchers shifted their focus to the origin of 
the dissolved charcoal. 

In an almost serendipitous scientific journey, Dittmar, head of the Max Planck 
Research Group for Marine Geochemistry at the University Oldenburg in Germany, 
was also tracing the paths of charcoal, but from an oceanographic perspective. 

To map out a more comprehensive picture, the researchers joined forces. Their 
conclusion is that charcoal in soils is making its way into the world's waters. 

"This study affirms the power of large-scale analyses made possible through 
international collaborations," says Saran Twombly, program director in NSF's 
Division of Environmental Biology, which funded the research along with NSF's 
Directorate for Geosciences. 

"What started out as a puzzling result from the Florida Everglades engaged 
scientists at other LTER sites in the U.S., and eventually expanded worldwide," 
says Twombly. "The result is a major contribution to our understanding of the 
carbon cycle." 

Fire is probably an integral part of the global carbon cycle, says Dittmar, its 
effects seen from land to sea. 

The discovery carries significant implications for bioengineering, the 
scientists believe. 

The global carbon budget is a balancing act between sources that produce carbon 
and sources that remove it. 

The new findings show that the amount of dissolved charcoal transported to the 
oceans is keeping pace with the total charcoal generated by fires annually on a 
global scale. 

While the environmental consequences of the accumulation of black carbon in 
surface and ocean waters are currently unknown, Jaffe said the findings mean 
that greater consideration should be given to carbon sequestration techniques. 

Biochar addition to soils is one such technique. 

Biochar technology is based on vegetation-derived charcoal that is added to 
agricultural soils as a means of sequestering carbon. 

As more people implement biochar technology, says Jaffe, they should take into 
consideration the potential dissolution of the charcoal to ensure that these 
techniques are environmentally friendly. 

Jaffe and Dittmar agree that there are still many unknowns when it comes to the 
environmental fate of charcoal, and both plan to move on to the next phase of 
the research. 

They've proved where charcoal goes. 
[RWL10: I am not so sure of this. The Masiello perspective has a graph showing 
CO2 release, never mentioned by Jaffe etal. I have no other concerns about the 
NSF press release.] 

Now they'd like to answer how that happens, and what the environmental 
consequences are. 

The more scientists can understand the process and the environmental factors 
controlling it, says Jaffe, the better the chances of developing strategies for 
carbon sequestration and mitigating climate change. 

The research was also conducted at NSF's Bonanza Creek; Konza Prairie; Hubbard 
Brook; Coweeta; and Georgia Coastal Ecosystems LTER sites, and at other 
locations around the world. 

Other authors of the paper are: Yan Ding of Florida International University; 
Jutta Niggemann of the Max Planck Research Group for Marine Geochemistry; Anssi 
Vahatalo of the University of Helsinki; Aron Stubbins of the Skidaway Institute 
of Oceanography in Savannah, Georgia; Robert Spencer of the Woods Hole Research 
Center in Massachusetts; and John Campbell of the USDA Forest Service. 

-NSF- 



Media Contacts 
Cheryl Dybas, NSF (703) 292-7734 [email protected]<mailto:[email protected]> 
JoAnn Adkins, FIU (305) 979-5276 [email protected]<mailto:[email protected]> 
McOwiti Thomas, LTER Network Office (505) 277-2638 
[email protected]<mailto:[email protected]> 

Related Websites 
NSF Publication: Discoveries in Long-Term Ecological Research: 
http://www.nsf.gov/pubs/2013/nsf13083/nsf13083.pdf?WT.mc_id=USNSF_25&WT.mc_ev=click
 
NSF Long-Term Ecological Research (LTER) Network: 
http://www.lternet.edu<http://www.nsf.gov/cgi-bin/good-bye?http://www.lternet.edu>
 
NSF Florida Coastal Everglades LTER Site: 
http://fce.lternet.edu/<http://www.nsf.gov/cgi-bin/good-bye?http://fce.lternet.edu/>
 
NSF Bonanza Creek LTER Site: 
http://www.lternet.edu/sites/bnz<http://www.nsf.gov/cgi-bin/good-bye?http://www.lternet.edu/sites/bnz>
 
NSF Konza Prairie LTER Site: 
http://www.lternet.edu/sites/knz<http://www.nsf.gov/cgi-bin/good-bye?http://www.lternet.edu/sites/knz>
 
NSF Hubbard Brook LTER Site: 
http://www.lternet.edu/sites/hbr<http://www.nsf.gov/cgi-bin/good-bye?http://www.lternet.edu/sites/hbr>
 
NSF Coweeta LTER Site: 
http://www.lternet.edu/sites/cwt<http://www.nsf.gov/cgi-bin/good-bye?http://www.lternet.edu/sites/cwt>
 
NSF Georgia Coastal Ecosystems LTER Site: 
http://www.lternet.edu/sites/gce<http://www.nsf.gov/cgi-bin/good-bye?http://www.lternet.edu/sites/gce>
 



The National Science Foundation (NSF) is an independent federal agency that 
supports fundamental research and education across all fields of science and 
engineering. In fiscal year (FY) 2012, its budget was $7.0 billion. NSF funds 
reach all 50 states through grants to nearly 2,000 colleges, universities and 
other institutions. Each year, NSF receives about 50,000 competitive requests 
for funding, and makes about 11,500 new funding awards. NSF also awards about 
$593 million in professional and service contracts yearly. 

[http://www.nsf.gov/images/mail_icon.gif] Get News Updates by Email 
<http://service.govdelivery.com/service/subscribe.html?code=USNSF_51> 

Useful NSF Web Sites: 
NSF Home Page: http://www.nsf.gov 
NSF News: http://www.nsf.gov/news/ 
For the News Media: http://www.nsf.gov/news/newsroom.jsp 
Science and Engineering Statistics: http://www.nsf.gov/statistics/ 
Awards Searches: http://www.nsf.gov/awardsearch/ 


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