- Author: Emily Baumstinger
UC Sierra Foothill REC is hosting a community workshop & field demonstration event where The Silver Lab at UC Berkeley will discuss results from a long-term (10 year) compost addition trial on foothill rangeland and observed benefits for forage quality, quantity, and soil health characteristics.
At this event, researchers will also be spreading compost for a new project supported by the 2017 Healthy Soils Demonstration Project and funded by Greenhouse Gas Reduction Funds and part of California Climate Investments.
- Demonstrate application of green waste and food waste compost
- Examine impacts of compost addition on forage production and quality
- Discuss how compost addition can improve rangeland soil properties
- Explore sourcing and applying compost at an operational scale
- Review cost/benefits and incentives
All are welcome to attend - Get more info by calling 530-639-8800 or emailing Jeremy James at firstname.lastname@example.org.
Date: Wednesday, November 14, 2018
Time: 10am – 12pm
Location: 8279 Scott Forbes Rd. Browns Valley, CA
- Author: Lauren Hallett
- Author: Katharine Suding
Over the last few years Californians have grappled with how to manage lands during times of both drought and plentiful rainfall. At SFREC and on Central Valley rangelands, one question is whether management that promotes high forage in wet years alters ecosystem resilience in dry years. For example, promoting highly productive grasses is a common goal. While drought years can negatively affect productive grasses, less productive species, particularly forbs like filaree, do relatively well in drought years due to decreased competition. Over the last several years the Suding lab and SFREC crew have been building ever-larger drought manipulations to test how different management practices, and associated species mixes, affect forage across good and bad rainfall years.
In the first iteration of this project, we looked at how grazing practices and rainfall interact to affect forage over dry and wet years. We hypothesized that grazing practices that maintained a diverse mix of grasses and forbs would promote more stable forage across wet and dry conditions. To test this, we first varied grazing intensity over four years within a pasture to describe how grazing alters grass and forb abundances (Figure 1a). Second, we implemented rainout shelters and irrigation over three years to create “dry” and “wet” plots within areas of different grazing histories (Figure 1b). We found that moderate grazing practices maintained a diverse mix of grass and forb species. This mixture better maintained vegetation cover and biomass across rainfall conditions compared to low-grazed areas dominated only by grasses (Figure 2) (Hallett, Stein, Suding conditionally accepted, Oecologia).
In the second iteration of this project, we are exploring how rainfall timing alters grassland diversity and forage production. We hypothesized that early-season drought will alter which species recruit that year, with higher forb abundance in dry falls and higher grass abundance in wet years, whereas late-season drought would reduce overall production. To test this, we have implemented large shelters with roofs that are pulled in place to create early-season, late-season and continuous drought as well as a control (Figure 3). We are finding that periodic early-season drought helps to maintain forb diversity in California rangelands. Working with Dr. Whendee Silver, we are also testing the effect of rainfall timing on nutrient cycling and greenhouse gas emissions. We are finding that previous-season rainfall as well as current season alters greenhouse gas emissions, which may be important for managing rangelands for multiple ecosystem services going into the future.
- Author: Nikolai Schweitzer
The Sierra Foothill Research and Extension Center in Browns Valley, CA utilizes 130 acres of summer irrigated pasture for cattle grazing. SFREC's irrigation water is supplied by a local water district via pipelines and open ditch distribution sources. The irrigation delivery system applies water through sprinklers, open ditches, and gated pipes. Each irrigated pasture at SFREC is managed for 1) Forage Production, 2) Water Quality, and 3) Soil Quality.
SFREC staff measures forage production in 15 enclosed cages throughout five different irrigated pastures. The treatments within each cage include leaving 4-6 inches of residual grass and measuring Total Forage Production (TFP). Guidelines for general irrigation and pasture management production based on past and current research recommend leaving 4 to 6 inches of residue/grass growth after each grazing period. The basis of this recommendation is to increase forage production (by leaving increased amounts of foliar surface area), improve root development, decrease weeds, cause less stress for forage grasses and increase water infiltration. Total Forage Production is measured by clipping the grass all the way to the ground. This center project is measuring the two treatments (4-6 inches & TFP) on their respective pounds/acre production. Each month (from April through October) forage is clipped from each cage, dried, and weighed (pounds/acre). After the samples are clipped, each enclosed area is leveled to its prescriptive treatment.
During the last two years of field sampling on irrigated pasture at SFREC, there was an increase in forage diversity in the Total Forage Production subplot. Clovers, birdsfoot trefoil, and filaree became increasingly abundant due to the increased sunlight and less crowding from competitive grasses. While the increase in clover and other forbes growth lends to an increase in forage quality, there is an overall decrease in forage production per acre in the TFP treatments when compared to the treatments with 4-6 inches of residual grass.
Numerous other factors can potentially impact irrigated pasture forage growth. Fertilization (rates, composition, timing), irrigation (frequency, amount, duration), grazing (stocking density, class/age of animal), species composition, physical structures (water location, loafing areas, rubbing zones, mineral location), soil properties, aspect, and slope, are other important components to manage or consider.
- Contributor: Megan G Osbourn
- Author: Jeremy James
Assembly member James Gallagher, who has strong ties to local agriculture in the Sacramento Valley, kicked off the day with a forward looking key-note address that highlighted the important role the current generation of students will play in addressing California's agricultural and natural resource needs over the coming decades.
Sponsors including Robinson Ranch, Farm Credit West and Yuba-Sutter Farm Bureau and the time donated by FFA leaders and UC staff were instrumental in making the second year of this annual event a major success and a great opportunity for students to interact with ongoing research led by UC.
- Author: Dan Macon
One of the most obvious signs of systemic stress, at least to me, are the water levels in our foothill reservoirs. After the first three years of this drought, we went into last winter with depressingly low water levels in most of our man made lakes. These reservoirs are critical for storing water for irrigation, human consumption, and downstream wildlife habitat. In normal years, they allow us to capture snow runoff and save it for use during the dry summer months. The winter of 2014-2015, however, brought virtually no snow to the Sierra Nevada – and consequently no spring runoff. I thought our reservoirs were low last summer; this summer is even worse. Last weekend, I drove across the Parrotts Ferry bridge over New Melones Reservoir (on the Stanislaus River between Calaveras and Tuolumne Counties). I was shocked to see that the water level had dropped below the old Parrotts Ferry bridge – I'd ridden across it as a kid, but didn't think I'd ever see it again once the New Melones Dam was built. Perhaps even more shocking – I could see the Stanislaus River flowing under the bridge.
Closer to home, the oak trees in Auburn and at the Sierra Foothill Research and Extension Center are starting to turn color as if autumn were already here. When deciduous trees experience extremely dry conditions, they'll often shed their leaves early as a survival mechanism. The blue oaks and black oaks at SFREC are dropping leaves earlier this year than most of us can remember. Some of the trees are in full color; they make the hillsides seem like we're already in October. In addition to turning color and dropping leaves, we've seen more trees dropping entire branches (and some are even falling down entirely).
According to the National Weather Service, one of the strongest El Niños ever measured seems to be shaping up in the Pacific Ocean. Many in the media are reporting this phenomenon as if it's a sure bet – our drought is all but over! Unfortunately, the impacts of El Niño aren't so certain – Northern California is just about as likely to experience dry conditions as wet weather in an El Niño year. I'll believe we're having a wet winter when I'm still wearing my mud boots next April! In the meantime, I'll keep an eye out for additional signs of stress.