These methods, instrumentation and/or protocols apply to all data in this dataset:Methods and protocols used in the collection of this data package |
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Study System
This work was conducted at the Cedar Creek Ecosystem Science Reserve (CCESR), a U.S. Long Term Ecological Research (USLTER) site located in central Minnesota, USA (Latitude 45.4 N, Longitude 93.2 W). The site has a mean annual precipitation of 750 mm and a mean annual temperature of 6o C (1970-2000)(Borer et al., 2014, Hijmans et al., 2005). Its soils are classified as marginal, given the dominance of sand (> 90 % sand in upland soils), rapid drainage, and low N levels compared to other grasslands (Fay et al., 2015, Grigal et al., 1974). Sand-dominated soils are widespread in North America especially in glacial outwash areas including Minnesota, Wisconsin, Michigan, Ontario, and the coastal plains of the southwestern USA (Liu et al., 2013). These soils are some of the least productive agricultural land on the continent, typically with low yield-to-input ratios, and are commonly targeted for land retirement (e.g., Plantinga, 1996). Accordingly, many of the areas at this site are abandoned agricultural fields (Isbell et al., 2019, Knops & Tilman, 2000).
At our study site, previous work has shown that long-term nutrient addition increased plant biomass and soil C, while reducing plant richness and shifting species composition from native C4 grasses to exotic agronomic C3 grasses (Clark & Tilman, 2008, Fornara & Tilman, 2012, Isbell et al., 2013). The reduction in plant richness was associated with a weakening effect of nutrient addition on plant biomass over the first 25 years of the experiment (Isbell et al., 2013). While nutrient addition had increased soil C by 27 years after tilling (Fornara & Tilman, 2012), the rate at which the gains in soil C accrued over this period remains unknown. In addition, it remains unknown whether the weakened fertilization effect on plant biomass – and continued decline in plant diversity – has slowed the accumulation of soil C during the decade since Fornara and Tilman (2012) examined the soils in these fields (years 25-37).
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Experimental Design
The experiment was replicated in three abandoned agricultural fields that were last tilled and farmed in 1968 (Field A), 1957 (Field B), and 1934 (Field C). All fields in this experiment are located on soils of the Sartell or Zimmerman series (Typic or Alfic Udipsamments, respectively) (Grigal et al., 1974). Detailed field descriptions are available in Tilman (1987). These timelines of abandonment for Fields A-C follow widely observed trends of land retirement of sand-dominated soils in North America; many areas were abandoned soon after cultivation (e.g., 1930s) while others maintained crop production for decades supported by higher-than-average nutrient inputs, more fine-tuned crop selection (e.g., tobacco), and periods of high crop prices that made these lands profitable (Feng et al., 2006). Ultimately, however, sandy soils like those in this study are often targeted for retirement given the high chemical input costs to maintain crop productivity and associated environmental impacts, erosion risks, and sensitivity to drought (Rey Benayas et al., 2007).
Prior to the experiment, each of the fields was enclosed by a 1.8 m tall wire fence with 10 cm openings. In addition, woven wire fence with 6 mm openings was buried 84 cm in the ground and extended 60 cm above the ground. In April 1982, two 35 x 55 m areas were designated in each of the three fields (A, B, and C). These areas were tilled with a 45 cm diameter disk harrow pulled by a tractor 20 times in one direction, 20 times perpendicularly, and 5 times diagonally. Following the disking, the soil was raked smooth and all remaining vegetation was removed. After tilling, the area was divided into 54 4 x 4 m plots with 1 m buffers between each plot. Aluminum flashing was buried to depth of 30 cm around each plot to prevent horizontal movement of nutrients and spreading of plants through vegetative growth. There have been no manipulations of the plant community (e.g., seeding or removal of plants) in any of the plots.
Following soil disturbance, a nutrient addition treatment was initiated with nine levels representing different combinations of nitrogen (0 – 27.2 g N m-2 yr-1 added as NH4NO3) and other non-N nutrients (20 g m-2 yr-1 P205; 20 g m-2 yr-1 K20; 40 g m-2 yr-1 CaCO3; 30.0 g m-2 yr-1 MgSO4; 18 microgram m-2 yr-1 CuSO4; 37.7 microgram m-2 yr-1 ZnSO4; 15.3 microgram m-2 yr-1 CoCO2; 322 microgram m-2 yr-1 MnCl2; and 15.1 microgram m-2 yr-1 NaMoO4) applied annually. In this design, there was one treatment with no nutrients (Control) and eight treatments that received non-N nutrients in combination with eight different levels of N (0 – 27.2 g N m-2 yr-1). The complete list of treatments is presented in Table S1. All nutrient treatments were replicated on the tilled and disked soils six times in a completely randomized design in each of the three fields (Figure S1).
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This method step describes provenance-based metadata as specified in the LTER EML Best Practices.
This provenance metadata does not contain entity specific information.
| Data Source | |
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This method step describes provenance-based metadata as specified in the LTER EML Best Practices.
This provenance metadata does not contain entity specific information.
| Data Source | |
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This method step describes provenance-based metadata as specified in the LTER EML Best Practices.
This provenance metadata does not contain entity specific information.
| Data Source | |
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This method step describes provenance-based metadata as specified in the LTER EML Best Practices.
This provenance metadata does not contain entity specific information.
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