Showing posts with label land. Show all posts
Showing posts with label land. Show all posts

Sunday, March 30, 2008

Soil organisms help ranchers

Intense, low duration grazing builds soil vitality, and increases soil organic matter.

Formulaically, the process described by Manske is very simple; what happens as a result is not.

A rancher chooses three pastures on which to graze the cattle. Starting in the first pasture, the cattle graze for 15 days, and then move on to the next pasture. This is repeated and the cattle find themselves in the third pasture.

Once the cattle leave the first pasture, the soil organisms go to work, converting the organic nitrogen into mineral nitrogen and feeding the plants, building their crude protein.

“Just by changing the management from focusing on dry matter poundage to managing those soil organisms, you can increase the productivity of your land,” Manske said. (Source)

Well observed.

Rhizosperic soil can get awfully puny under long duration grazing. Topsoil pales and topsoil depth is lost, but not to sediment discharge or wind erosion. The in-situ transformation of topsoil to not-topsoil results in the discharge of soil carbon to the atmosphere. The good news is that, unlike wind erosion, water erosion, sheet erosion, or gully erosion erosion, this yet-to-be-named variant of topsoil erosion is reversible.

Monday, September 10, 2007

Sunnyside Wetland


One of my projects made the front page of the Yakima newspaper. Since the paper tends to paywall these things in short order, I thought the blog would make a handy archive.

The picture here is from the project site. The retaining wall in the picture was placed by the county in order to keep the road apron from impacting what was presumed from USFWS-NWI reconnaisance mapping to be a jurisdiction wetland. That mapping plus the observed standing water and the wetland vegetation seemed to the county to be proof positive that clearing the land was a violation of the county critical areas code. It wasn't.


Published on Monday, September 10, 2007

County learns lessons from fight with farmer
By PAT MUIR
YAKIMA HERALD-REPUBLIC

SUNNYSIDE -- Don Young didn't think his neighbor's irrigation water leaking into his property should qualify it as wetland, and after a yearlong fight, Yakima County agreed with him.

The saga, which Young documented in a meticulous inch-thick file he says makes him feel like an attorney, cost him about $6,000 by his count and kept him from using the land until last month. It also forced county leaders to rethink the way they apply the county's Critical Areas Ordinance. The ordinance, which has been under review for five years and is nearly finished, still will be enforced as mandated by state law, county Public Services Director Vern Redifer said.

"But where you can construe the law in the favor of property owners, we'll construe it that way," he said.

That's good news to Young, a self-described "stubborn old farmer" who believes he might not have prevailed in his dispute if he hadn't had the money for a consultant to make his case.

"This is a story that needs to be told, not for my benefit but for the taxpayers and the public," the 73-year-old retired rancher said.

The whole thing began when a county road crew spotted Young pulling up vegetation on the edge of his property. The county issued a cease-and-desist order in May 2006, about seven months after Young bought the 4-acre property south of Sunnyside. To his thinking, the Russian olive trees and other vegetation he removed were just trash like the piles of tires and garbage that were also on the property.

Thinking he was actually improving the land, Young took umbrage to the county's order, which included the possibility of $1,000-a-day fines.

"Nobody ever said anything about it being a wetland," he said.

He also didn't like the way county staff treated him when he disputed the matter. It was clear enough to Young that the land in question wasn't a wetland because the only source of water was the neighbor's irrigation runoff, or what his hired consultant labeled "water trespass." But he couldn't get the county to see it that way.

"The heading of their letter is 'public services,'" Young said. "I told them they need to change that, because there is no way in this world that they are serving the public."

The county's opinion on the matter didn't change until Young received a report he'd commissioned on the matter by wetlands delineation expert Phil Small of Spokane. Small's report, written after a visit to the property during which he drilled holes to measure groundwater levels, found there was no source of water other than the irrigation runoff. The county considered it a persuasive argument and in a July 31 letter lifted the cease-and-
desist order.

"What I want to know," Young said, "is why didn't the county have to hire him to prove it was a wetland instead of me having to hire him to prove it's not."

In the county staff's defense, the property did have signs of being a wetland, such as reeds, bulrushes and the Russian olive trees, Redifer said. The staff was simply following its procedures as laid out in its own policy and didn't err in that regard, he said.

County officials tried to work with Young along the way, planning manager Steve Erickson said. But the county's suggestion that Young "wait and see" if his property was a wetland based on whether groundwater returned even without irrigation runoff didn't fit into Young's schedule, Erickson said. That meant Young had to hire his consultant to force the issue, but that was up to him, Erickson said.

Where things might have been done differently, and will be in the future, is in the way county staff deals with people in such disputes, Redifer said.

Comparing it to baseball, in which "ties go to the runner," he said if there are questions about whether to act on a possible wetland scenario like Young's, the landowner will be "the runner." That is in line with the Yakima County Commissioners philosophy of a more user-friendly Critical Areas Ordinance application, which they have espoused during deliberations on the ordinance.

Staff also might call people in the future or knock on their doors, rather than sending formal letters specifying possible fines.

"I think (the letter) made him feel like a big lawbreaker, and that certainly wasn't the intent," Redifer said.

"That's another lesson learned -- how we go about engaging someone with a potential violation," Erickson added.

While he would be happy to see such changes, Young still isn't sure the county has done right by him. He's contemplating filing a claim to recoup the money he spent fighting the initial ruling. In the meantime, though, he's working the land for the first time in about a year.

He's put manure down and hopes to have the whole thing seeded for pasture by the end of September.

"I lost the production of that land for a year already," he said. "Over a year."

* Pat Muir can be reached at 577-7693 or pmuir@yakimaherald.com.

Wednesday, May 09, 2007

Biofuel demand pencils out to damaged soil

Crop residue is not a waste. It is a precious commodity and essential to preserving soil quality.

Production systems must be developed so that ethanol produced must be at least C neutral if not C negative. Temptations [to mine soil vitality] aside, biofuels produced from crop residues may neither be free nor cheap.
Rattan Lal, SSSA President, has a timely message to his fellow Society members in the May issue of CSA News (regretfully subscription only). It is that we must take this opportunity to break the cycle of soil destruction that characterizes the rise and fall of civilized man. Biofuels adds unprecedented value to biomass production. Rattan Lal sketches out the numbers, comparing potential demand to crop residue available. With demand tracking above supply, the temptation is to mine the soil of its vitality. Rattan Lal observes that soil exploitation is the primary contributing factor to desertification.
Harvesting crop residues for use as fodder for livestock, residential fuel for cooking and heating, construction material, and other competing uses is a reality in sub-Saharan Africa, South Asia, China, and other developing countries. Therefore, it is not surprising that these are also the regions that have been plagued with severe problems of soil degradation.

With a severe decline in physical quality, degraded soils do not respond to fertilizers even if made available at a subsidized price. Adverse effects of none or low rates of applications of fertilizers and other amendments on agronomic production and soil quality have been exacerbated by the perpetual and indiscriminate removal of crop residues coupled with uncontrolled and excessive communal grazing.

The stubborn trends of low crop yields and perpetual hunger and malnutrition in sub-Saharan Africa and in regions of rainfed agriculture in South Asia cannot be reversed without returning crop residues to the soil and also supplementing them with liberal applications of other biosolids.
Rattan Lal has done an admirable job in this appeal to the his fellow SSSA members. He has included constructive comment on tools and processes available to make biofuels production compatible with maintaining soil vitality. But the undercurrent message is that those of us who love soil must involve ourselves in the process, the policy, and the public discussion of our transition to sustainable energy.

Leave comment or email me if you would like to request a copy of Rattan Lal's May address. Or better yet, join SSSA.

Wednesday, February 14, 2007

Soils and its role in a changing climate

Roger Pielke Sr., over at his research group's climate science blog, has been holding forth on land use change and its impacts on long-term near surface temperature. His position is that the role of land use must be further emphasized within the climate change framework. Search for "soil" and "land" for a long list of supporting posts.

This goes beyond deforestation and urban heat islands. Dust and alterations in atmospheric water content play unknown roles and interact with albedo in sometimes counterintuitive ways. For example, irrigation warms rather than cools the land. Evaporative cooling is insufficient to drive net cooling of irrigated regions. Soils darkened by moisture absorb more heat than dry soils and re-radiate more heat during the night. This results in warmer nights and warmer average temperatures.

Current climate models are not sensitive to changes in land use. Neither are they sensitive to the soil's role in affecting atmospheric carbon levels.

Soil organic matter, at roughly 1500 GtC, is the single largest compartment of carbon in the active biogeochemical cycle. At 60 GtC annual flux (in either direction), it is 10 times larger than the 5.5 GtC flux due to burning fossil fuel. Yet soil is the component of the carbon cycle that we know the least about.

Most soil scientists agree with the unvalidated concept that soil carbon levels will likely decline in step with temperature increases. Higher biological activity will result in more decomposition of organic matter. One certainly sees a similar relationship between soil carbon and temperature when comparing the effect of elevation, aspect and latitude. That we have yet to validate it is telling.
Current climate models mostly ignore the specific role that soil microbes play in the release of carbon dioxide into the atmosphere. The information they do include is often based on assumptions that have never been tested in the field, and may be wrong or overly simplistic.
Our climate models are telling us we need to become far more efficient and more conservative in managing our planet's carbon, soil-wise and fuel-wise. But our scientific understanding will never be adequate for crafting our full response to climate change.
The fact is that our climate is infinitely complex. The models climatologists use to predict the future are incredibly sophisticated, yet blunt instruments. Scientists can never account for all the variables involved - indeed, no one has successfully come up with a mathematical equation to describe the formation of a single cloud. And scientists are often woefully out of their depth in the real world. History is littered with lives and regimes that were wrecked when science was allowed to drive policy with no thought to humanity. Tearing down the global carbon-based economy to - in theory - replace it at a later date with unproven and undeveloped technologies would be a similar folly. It is only by tempering science with economics and the market, which is the most efficient arbiter of humanity's wants and needs, that smart climate policy can be made.
Science and the market are partners of longstanding. Economic necessity, as the mother of invention, has been driving the advance of science for as long as science has been an identifiable pursuit.

Distorted Vision
Originally uploaded by uaezlulu.

Tuesday, January 23, 2007

NRCS Assessment of US Land Use, Erosion, Wetlands

The USDA Natural Resources Conservation Service has posted results of their Natural Resources Inventory (NRI). Depicted are land cover and use, soil erosion, and wetland gains or losses for the 48 contiguous United States.

From 1977 to 1997, NRCS conducted the assessment every five years, in 2000, they began the transition to an annual assessment. The most recent data is from 2003 and reflects only conditions at that point, NRCS Chief, Arlen Lancaster says, "This is a snapshot, this is the number in terms of cropland, this is where we're at in terms of erosion," he says later this year they will be able to provide numbers that reflect the change from year-to-year.

Some findings:

  1. The 48 contiguous states cover 1.9 billion acres and 71% of that, 1.4 billion is in non-Federal rural land uses. Of that 1.4 billion acres, 406 million is in forest land, 405 million is rangeland and 368 million is cropland.
  2. Cropland acreage decreased 12% from 1982 to 2003. The net decline between 1997 and 2003 was 8 million acres, or about 2 percent.
  3. Soil erosion on U.S. cropland decreased 43% from 1982 to 2003.
  4. In 1982, 40% of all cropland was eroding above soil loss tolerance rates, that number declined to 28% in 2003.
  5. Erosion rates on a per acre basis declined significantly between 1982 and 2003. Sheet and rill erosion on cropland dropped from 4.0 tons per acre per year in 1982 to 2.6 tons per acre per year in 2003; wind erosion rates dropped from 3.3 to 2.1 tons per acre per year.
  6. There was a net gain in wetland acres on non-Federal rural lands between 1997 and 2003. Annual net gains between 2001 and 2003 were 72,000 acres per year, of which 44,000 acres per year were on agricultural lands.

The 2003 results look fairly encouraging. Erosion continued down. There was a net gain in wetland acres coming substantially from agricultural lands and a moderated trend of farmland loss. It fits with what I was seeing on the ground in those years. 2004, 2005 and 2006 might not be as good as 2001 - 2003. Funding for soil conservation and especially wetland construction was tighter after 2003. This was also at a time when tiling was on the increase, as I reported earlier. The farmland loss rate probably regained some steam with development activity. Any comments?


Sunday, February 12, 2006

Grazing tool for managing riparian buffers

A Capital Press article (subscription) by Doug Warnock promotes grazing in riparian buffer areas, saying:

When grazed properly, forage plants in the riparian zone can be stimulated to re-grow and contribute greatly to the health of the ecosystem.
The grazing process helps break up capped soil...
Up until a few months ago I was enthusiastic about preserving soil crusts. Some reasoned criticism of this perspective has helped moderate my opinion.
... stimulates the incorporation of plant tissue into the soil resulting in increased organic matter and the animals add minerals to the soil. It also helps control the growth of woody plants, which can shade out desirable grasses and forbs that hold the soil on stream banks and filter out soil particles during high water periods. Grazing animals can also be effective in controlling undesirable plants, if grazed at the proper time.
By excluding this tool (grazing), other tools must be used in to manage the property and most of them are more costly. Herbicides to control weeds, and equipment to cut back brush and trees require out-of-pocket expenditures. Still, probably the most important benefit from grazing is the stimulation of the growth of the grasses and forbs by the removal of part of the plants’ stems and leaves.
The key, in all of this, is to not allow the grazing animals unlimited access to the riparian zone, so that they are kept from overgrazing the plants.
This all makes good sense and the article goes on to line out the tools available to make it happen. In comparison, the common regulatory default position of universally excluding the total sum of all excludable activity from all riparian buffer areas appears a convenient stop gap rather than a reasoned construct.

Thursday, February 09, 2006

My field season begins...

...with soil sampling at a waste water irrigated hay field. The study site has high gravel content which is farly well sorted due to the action of glacial age Missoula floods. In the picture, the AMS tile probe helps locate high gravel content areas to avoid sampling. The AMS mud bucket auger has wide-set teeth that accommodates the smaller gravels. The 0.25 inch screen helps reduce the sample for shipping. The screen also aids in mixing the sample prior to reduction.

Soil scientists required in Pennsylvania for septic system permits

Soil scientists at work. In many states, professional soil scientists conduct the septic system site assessments required for permit approval. Soil scientists also get involved in adapting alternative on-site disposal technologies. This brief newspaper interview with Leonard Cornish, owner of Pocono Soil and Environmental Consulting Inc., Wilkes-Barre, PA reveals some of the basic scientific and technical requirements needed in this type of a business. The news article should be of particular interest to soil scientists considering going into the business of environmental consulting or individuals looking to hire on with a soil scientist owned business.


Sunday, February 05, 2006

Farm tile drainage progressing rapidly (II)

As mentioned here earlier, farm tile drainage is being linked to accelerated wetland loss in Minnesota. A meeting held Saturday, February 5, to discuss wetland loss drew a crowd of 300. One person testified that “99 - 100%” of the wetlands in his county were now gone. Details are reported in the St. Paul MN Pioneer Press article with the headline: “Get tough to protect wetlands, group says”. Reading the tone of the reporting, it confirms my earlier impresssion that the majority of the wetland loss is considered to be due to draining uplands adjacent to wetlands. My read (see pdf addressing MN wetland regs) is that this is normally a legal undertaking. Installing drain tile within a wetland would not be legal. This foreseeable cause of wetland loss, due to activities outside of wetlands, seems to have caught wetland advocates without a workable strategy.


Dry lab fraud alleged

Have you taken soil samples and tested soils to determine the level of plant available nutrients in the soil?

Question No. 1, page 12, Self-Assessment Workbook (pdf)

Most soil lab procedures involve wet chemistry. Dry lab results, in the vernacular, are made-up results, place-holders if you will. Sometimes they serve a legitimate purpose. Dry labbing with the intent to deceive for monetary gain is fraud. This is apparently what USDA-NRCS is accusing 15 unnamed eastern Washington farmers of when they self-qualified for monetary awards under the Conservation Security Program. CSP participants in the top tier receive up to $45,000 per year for a 10 year period for the most environmentally conscious farms. Reading both the linked Seattle P-I article and the original Spokesman-Review article, (subscription required) it looks like a few farmers fabricated a history of soil sampling and lab analysis in order to qualify. The good news is that 131 farmers audited came up clean.

For other CSP news, see also:
Capital Press article (subscription required): “CSP losing momentum”
Delta Farm Press
article: “USDA announces cut in CSP watersheds in 2006”

Wednesday, February 01, 2006

Precise common sense II

Elton Robinson expands nicely on the previous post by email:

The variable-rate application of inputs is actually well developed and prospering in Mid-South cotton fields. It works for two reasons. One, we have highly variable soils along the Mississippi River Delta, which in turn creates variable yields. Second, the cotton crop demands intense in-season management for plant growth, insects, weed management, disease and harvest preparation.

Infrared aerial photography and electrical conductivity mapping carts can pick up the variation in soil type when the ground is bare and pick up plant biomass when the crop is growing. Geo-referenced maps generated from the imagery allow the farmer to vary applications of plant growth regulator, defoliants and other inputs during the season based on variability in biomass. For example, the poor-yielding parts of the field will receive less plant growth regulator to allow plants to catch up with the better-yielding parts of the field, which in turn will receiver more plant growth regulator, to prevent vegetative growth. The result is higher yield and lower cost.

The cost to the farmer for the imagery, and variable-rate prescription is $7 per acre. Sprayers can be adapted for variable rate applications for $6,000. The cost of producing cotton is about $500 an acre. A conservative savings in input costs of 10 percent plus a 5 percent increase in yield would put $65 an acre in the farmer’s pocket. If he farms 1,000 acres of cotton, that $65,000, more than enough to pay off the cost of the technology in year one.

The technology is not affordable if there is little variability in the soil, or if a crop (corn, soybeans) does not respond as well to in-season management. I did read your previous blog on VR nitrogen, and agree that it's been very difficult for researchers to show a benefit.

Tuesday, January 31, 2006

Precise common sense

Precision ag implies computer mapped lab data and GPS controlled field equipment. Higher yields, less flying blind and easier farming. The reality is that the expense of data collection, analysis and interpretation can quickly wipeout any added value. Reading this article about variable rate management of cotton, it struck me that common sense and curiosity are the missing ingredients. Elton Robinson with Delta Press reports on cotton producer Kenneth Hood, Mississippi, who attributes his success with variable rate agriculture to, among other things, reliance on aerial photo interpretation, an approach not typical of precision agriculture. Hood says that the “... advantage to imagery is that very little data collection is required, according to Hood, “which is unlike most precision agriculture practices.” Put this experience together with the recent cryptic news on the lukewarm record of precision agriculture in Germany, which I touched on earlier, and what do you get? My sense is that Kenneth Hood is going to have lots of company.

Sunday, January 29, 2006

Farm tile drainage progressing rapidly

As told by Chris Niskanen over at the St. Paul MN Pioneer Press there is a tremendous amount of tile drainage going on in the north central USA: 100 million feet per year or about 19,000 miles by one estimate. Improved flexible drain tile is making this unprecedented rate of installation possible. The article mentions a number of areas of potential concern: loss of duck habitat and increased nitrate levels in surface water. Where no jurisdictional wetlands are being tiled, no permits are needed to perform this work. However the extent of the practice has caught the attention of folks and a community effort to address the impact of farm drainage on wetland habitat is being discussed.
Image source: South Dakota State University – Ag environmental issues page
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Saturday, January 28, 2006

Tallahassee waste water sprayfield nitrate concern for Wakulla springs

I have been following news on a 2600 acre sprayfield on the edge of Tallahassee, Florida. It is suspected of causing environmental problems 10 miles away in Wakulla Springs State Park and the Wakulla River. A recent 1000 Friends of Florida report (pdf) ties excessive hydrilla plant growth to nitrate from the sprayfield. The news this week is that the city, USGS and Florida DEP will be conducting dye tests to better understand how the groundwater beneath the sprayfield moves down gradient. I am reading the report. Striking is the relatively low (1.0 mg/l)nitrate-N needed to control the situation.

Image source: Tallahassee Democrat


Thursday, January 26, 2006

Product review - new vadose zone research tool moves to farm

Irrigated farm fields lose water to deep percolation. This groundwater recharge, and what it contains, is difficult to research. This is because sampling tools designed to intercept saturated flow tend to miss unsaturated flow. And visa versa. New technology extracts deep soil moisture using a wick rather than the active suction or gravity.

The first wick samplers were passive capillary samplers (PCS). This approach has now evolved into the current water flux meter (WFM) designed recently by Batelle soil scientist Glendon Gee. Two offspring WFM designs are commercially available: the Gee passive capillary sampler drain gauge (Decagon Devices, Pullman WA) and the vadose zone water flux meter (Sledge Sales Consulting, Dayton OR). In a recent journal article, the Decagon device is referred to as a capacitance water flux meter (C-WFM) and the Sledge device is referred to as a tipping-bucket water flux meter (T-WFM). The T-WFM is close to Glendon Gee's designs published in journal articles. The C-WFM was developed by Decagon soil scientist Gaylon Campbell in collaboration with Glendon Gee.

The original PCS devices needed a pit, best dug with a backhoe. Fiberglass wick length and strand size were calibrated to site specific conditions to prevent oversampling of unsaturated conditions. Today's WFMs can be placed in an auger hole or hand-dug pit. WFM configurations use a standard size and length wick which works for most situations. A recent journal article has an example of an oversampling problem.

There are strong similarities and distinct differences between the two firms. Like Decagon, Sledge maintains strong ties with Glendon Gee. Like Decagon, many of the 200 devices Sledge has produced have been for agricultural research. Compared to Decagon, Sledge is more a hands on, farm service and farm chemical oriented consulting business. With Wayne Sledge, the T-WFM is his flagship product. With Decagon, the C-WFM is a sensible addition, part of an extensive and well supported line of soil and agricultural measurement instrumentation. It appears that Decagon and Sledge have produced a similar number of devices and they are clearly on parallel tracks of success in refining their individual product.

Both firms have supplied most of their instruments to agricultural researchers, farms and clients concerned with water use efficiency and nitrogen use eficiency such as golf courses. There has also been environmental project placements, most often associated with landfill and mine-tailing closure

Decagon has put considerable effort into refining unit capacity to record water flux, less into water sample handling. The larger base of the Sledge unit enhances water sample handling options. Decagon has a stepped design which accommodates hand auguring the deepest portion, shortening installation time. Decagon has an extensive list of complementary devices and highly capable technical support staff. The Sledge unit is substantially lower in price. Choice is good.

Of particular interest in Washington State is wastewater spray field management. As mentioned in a government report: "The Department of Ecology has identified 20 spray field situations where wastewater was [improperly] applied [and conditions] ... led to contamination of groundwater...". This report was discussed here previously.

I spoke with Don Nichols, with Washington Department of Ecology's Water Quality Program, Eastern Regional Office, Spokane, WA. Don has encouraged the installation of WFMs for gathering vadose zone water quality information. Don referred me to Cascade Earth Sciences and Soil Test Farm Consultants for more information.

Dan Burgard, soil scientist with Cascade Earth Sciences (CES) in Spokane, WA has installed 7 Decagon C-WFMs in the Pasco, WA area, and 11 Sledge T-WFMs in southern California. CES modified the equipment to enhance sample collection capabilities. (See his photos below)

Dan Nelson, soil scientist with Soiltest Farm Consultants, Inc. in Moses Lake, WA has four Decagon C-WFMs installed in the Moses Lake, WA area. Both had nothing but good things to say about the potential uses of this type of data. Mass balance calculations will demonstrate if target water use efficiency and target nitrogen use efficiency is being achieved. Detailed daily data logs show exactly when percolation occurs. Percolation events observed to date are closely correlated with irrigation and precipitation events and even soil thawing events. As expected with the difference in weight between soil and the field capacity water portion, percolate nitrate and dissolved solids (salts) are several times higher than soil levels above the sample point. The devices are performing as intended.

One question I have is how many devices are needed to achieve statistical confidence in a mass balance calculation? Users independently tend toward sets of 3 units, with singles for spot comparison data. That is a sensible starting point but determining coefficient of variability on selected data would put the results into perspective.


None of the installations have been entirely glitch-free, mostly due to various data logger challenges or site specific soil related factors, such as coarse sands or depth limits. Users of the units are looking forward to continued refinements in data logger compatibility and would like to see costs come down and but give high marks for ease of installation and setup. This and available tech support make sampler units from Sledge and Decagon an attractive alternative to the do-it-yourself installations that predate this equipment.


References:
Brown, K.W., J.C. Thomas, and M.W. Holder. 1986. Development of a capillary wick unsaturated zone water sampler. Coop. Agreement CR812316-01-0. USEPA Environ. Monit. Syst. Lab., Las Vegas, NV.
Cary, J.W. 1968. An instrument for in situ measurements of soil moisture flow and suction. Soil Sci. Soc. Am. Proc. 32:3–5.
Gee, Glendon W., Zhang, Z. Fred, Ward, Andy L. 2003. A Modified Vadose Zone Fluxmeter with Solution Collection Capability Vadose Zone J 2003 2: 627-632 (highwire link) http://highwire.stanford.edu/
Knutson, J.H., and J.S. Selker. 1994. Unsaturated hydraulic conductivities of fiberglass wicks and designing capillary wick pore-water samplers. Soil Sci. Soc. Am. J. 58:721–729.
Selker
, J.S., C.K. Keller, J.T. McCord. 1999. Vadose Zone Processes, Lewis Publishers, ISBN 0-87371-953-0, GB1197.7.S46 1999 [1] [2]
van der Velde, M., Green, S. R., Gee, G. W., Vanclooster, M., Clothier, B. E. Evaluation of Drainage from Passive Suction and Nonsuction Flux Meters in a Volcanic Clay Soil under Tropical Conditions Vadose Zone J 2005 4: 1201-1209 (DOI: 10.2136/vzj2005.0011) (highwire link)










Life and the look of landforms

Geomorphologists report surprising similarity in landforms on Mars with landforms on Earth, considering the importance that soil life has on landform processes. They conclude:
"Despite the profound influence of biota on erosion processes and landscape evolution, surprisingly,…there are no landforms that can exist only in the presence of life and, thus, an abiotic Earth probably would present no unfamiliar landscapes," said Dietrich.
URL: Life leaves subtle signature in the lay of the land - UC Berkeley
It's a thought provoking read, especially for those of us who interpret the land at the more arid end of the spectrum.

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Friday, January 20, 2006

German science workshop news critical of precision agriculture performance

A German soil science research center reports that Precision Agriculture has not delivered on promised benefits, stating:
...worse are the actually reported effects of ..."Precision Agriculture" (PA) ...on N efficiency. Still after 15 years of implementation no results proving consistent increases in yields or decreased fertilizer application are available. Quite the contrary: some of the techniques developed in PA may even decrease fertilizer N efficiency...
The Federal Agricultural Research Center (FAL) - Institute of Plant Nutrition and Soil Science's workshop, Options for reducing the nitrogen surplus in plant production, has individual presentation pdf files available, including the one on PA.


Monday, January 16, 2006

Tetany animal health issue and soil, hay links

Tetany is a complex disease in that no specific condition triggers it in all cases. Gauge tetany risk using soil and tissue analysis when growing or feeding hay comprised solely of cool-season grasses. A grass-legume mix does not have this risk.

Tetany is a disease affecting ruminants and is associated with feeding or grazing bluegrass, bromegrass, fescue, orchardgrass, ryegrass, timothy and wheatgrass. It is caused by low blood levels of calcium and/or magnesium. Classic risk conditions occur when the forage grass is growing quickly in the spring and nitrogen levels are high. Less well known is that tetany can be a problem when hay is grown on soils with excessive soil potassium. Manure and potassium hydroxide cleansers are two potential sources. Lactating animals are more susceptible to tetany, thus dairies are particularly alert to the concern and tend to avoid growing or feeding grass hay exclusively. Forage guides may not mention it as a concern. A forage tissue ratio of K/(Ca+Mg) of more than 2.2 indicates a high risk of tetany and the need to supplement feed with magnesium (Mg) (see also). If an animal goes down and tetany is suspected, a veterinarian should be contacted for immediate treatment. Often an animal will recover if it can be given an injection of magnesium sulfate (Epsom salts) early on.

Preventative Mg feed supplement and the ready supply of alfalfa tends to keep the incidence of tetany to a minimum. My thought is that tetany is additionally controlled by the close knit nature of farm communities. Caring neighbors and long memories tend to interact sufficiently that tetany symptoms don't take more than an animal or two, usually the weakest anyway, before it is figured out. Perhaps this explains why analytical laboratories in my region are generally unaware of tetany or the role of soil and tissue nutrient levels. My opinion is that cooperative extension publications in the Pacific Northwest can do better in this area. Tips for preventing animal loss due to tetany should be included in the fertility guides published to help folk interpret forage test results.

See also:
Spring Mineral Considerations by Jeff Heldt (link added 03MAR06)
Controlling Grass Tetany in Livestock, by Cooperative Extension, New Mexico State University, available in pdf format

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Saturday, January 07, 2006

Ida Powell


In southeast Yakima is a Carpathian walnut tree. It was planted long ago and the trunk is now 3-4 feet thick. It towers over the expansive 1895 farmhouse that it shades. Beneath its spreading branches, four huge picnic tables wait patiently for spring. That is when the neighbors will return, as they have every year since the early 1980's, to work alongside church and trade school volunteers to reawaken the proud building at the corner of Spruce and Union (Union is where 9th St. would be). Others work to rejuvenate the 1 acre of pioneer planting that helped qualify this Estate's placement on the State's Register of Historic Places. Restoring the property to the community is the vision of the South East Neighborhood Improvement Committee (SENIC), a 501c(3) non-profit corporation. SENIC's unofficial motto is "we can do more good with nothing than others accomplish with thousands." In support of SENIC's efforts at the Historic Ida Powell estate, a PayPal donations link is provided below. Please make a donation and please visit this summer to share in the project. Parcheesi players are especially welcome for late summer evening games in the shade of the walnut tree.




(Historic Property Inventory Form for this site - PDF )
(If you have MS Internet Explorer you can get to a nice write up and picture using the query function at the State Department of Archaeology and Historic Preservation's WISAARD site, but it takes some doing to get there. "Query" (lower Left) for POWELL HOUSE)

UPDATE: I neglected to mention that the POWELL HOUSE is also on the National Register of Historic Places)





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Friday, December 30, 2005

Indicator of Reduction in Soils (IRIS)

The list of activities and structures that don't do so well in reduced conditions is pretty long: septic drain fields, crops and steel underground storage tanks come to mind. On the other hand, reduced conditions are a requirement for jurisdictional wetland designation and constructed wetlands. Beyond that, watching the playoff between various redox gradients in soil is just plain fun.

Pedology and Wetland Soils

B. J. Jenkinson and D. P. Franzmeier*

Dept. of Agronomy, Purdue Univ., Lilly Hall of Life Sciences, 915 W. State St., West Lafayette, IN 47907-2054

* Corresponding author (dfranzme@purdue.edu )

Soil drainage conditions are important to land use decisions. Traditionally, anaerobic conditions induced by poor drainage have been evaluated by observing soil color related to Fe and Mn oxides, using {alpha}, {alpha}-dipyridyl dye, measuring dissolved O2, and measuring EH. We believe that there is further need for a device that is scientifically sound and easy to use. Therefore, our goals were to develop and test a device that mimics natural soil processes, visually indicates soil reduction, and is robust. Our concept was to coat a rod or tube with a colored soil mineral that dissolves on reduction, insert the device into a soil, remove it after a few weeks or longer, and observe if some of the coating had been lost. If the coating was not dissolved, no reduction occurred, but if it was dissolved, reducing conditions must have prevailed. After trying several kinds of coatings and tubes, we chose ferrihydrite (FH) coating on polyvinyl chloride (PVC) pipe. We call the device an Indicator of Reduction in Soils (IRIS). As the study progressed we added semi-quantitative interpretations by measuring depleted areas using a digital camera and image analysis. We tested IRIS tubes in the lab and in soils in Indiana, Minnesota, and North Dakota, and concluded they performed as expected. Reduction rates increased between February and April and were related to increasing soil temperature, turnover (flux) of soil OC, and content (inventory) of OC. Reduction rates decreased after April, presumably because the nutrient supply for microbes decreased.


Abbreviations: Ac, area of FH coating in contact with the soil • Ad, area from which some FH had been depleted • D, percentage of Ac from which some FH had been depleted • DO, dissolved O2 concentration • FH, ferrihydrite • IRIS, indicator(s) of reduction in soils • OC, organic carbon • PVC, polyvinyl chloride • UDD, upper depth of FH depletion


Easy and straightforward. Kind of like the traditional sticking of the toothpick into the banana bread to see if it's done.

Note: I updated this article a few hours after posting the original. If you read the first version, my sympathies. What can I say. Its a gift.

Further Reading:
Redoximorphic Features Powerpoint presentation developed by: Michael Whited, USDA-NRCS - Wetland Science Institute August, 2000. (4.6 MB) (source page )

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