Drought Resistant Soil


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Drought Resistant Soil

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Drought Resistant Soil

  1. 1. DROUGHT RESISTANT SOIL Agronomy Technical NoteAbstract: To minimize the impact of drought, soil needs to capture the rainwater that falls on it, store as much of thatwater as possible for future plant use, and allow for plant roots to penetrate and proliferate. These conditions can beachieved through management of organic matter, which can increase water storage by 16,000 gallons per acre foot foreach 1% organic matter. Organic matter also increases the soil’s ability to take in water during rainfall events, assuringthat more water will be stored. Ground cover also increases the water infiltration rate while lowering soil water evaporation.When all these factors are taken together the the severity of drought and the need for irrigation are greatly reduced.By Preston Sullivan port them. Any worthwhile strategy for droughtNCAT Agriculture Specialist management optimizes the following factors:November 2002 • Capture of a high percentage of rainfall (in- filtration) Table of Contents • Maximum storage of water in the soil for later use (water holding capacity) Introduction ................................... 1 • Efficient recovery of stored water (plant root- Texture ............................................ 1 ing) Aggregation ................................... 2 Several important soil factors affect water man- Organic Matter and agement—including soil texture, aggregation, Water-holding Capacity ........... 3 organic matter content, and surface ground Ground Cover ................................ 3 cover. Farmer Profiles .............................. 6 References ...................................... 6 Texture Texture refers to the proportions of sand, silt, andIntroduction clay present in a given soil. A sandy loam, for example, has much more sand and much lessWith severe drought an all-too-common occur- clay than does a clay loam. A loam soil is a morerence, some farmers turn to irrigation for a solu- balanced blend of sand, silt, and clay. Most soilstion. Irrigation may not be feasible or even de- are some type of loam. Texture is an innate char-sirable. Fortunately, there are management op- acteristic of the soil type. Unlike the other fac-tions that can increase the soil’s ability to store tors discussed here—aggregation, organic mat-water for plant use. Soil can be managed in ways ter, and ground cover—texture cannot bethat reduce the need for supplemental watering changed through agronomic practice. By know-and increase the sustainability of the farm. This ing the innate texture of the soil, however, thepublication details some of the strategies for farmer can select and adjust practices that opti-drought-proofing soil and the concepts that sup- mize moisture management.ATTRA is the national sustainable agriculture information service, operated by the National Centerfor Appropriate Technology through a grant from the Rural Business-Cooperative Service, U.S.Department of Agriculture. These organizations do not recommend or endorse products,companies, or individuals. NCAT has offices in Fayetteville, Arkansas (P.O. Box 3657, Fayetteville,AR 72702), Butte, Montana, and Davis, California.
  2. 2. Soil moisture-holding capacities corresponding Well-aggregated soil also resists surface crusting.to texture designations are found in Table 1. The impact of raindrops causes crusting onNotice that although the plant-available water is poorly aggregated soil by disbursing clay par-highest in the loam to clay-loam textures, the to- ticles on the soil surface, clogging the pores im-tal water goes up with increasing clay content. mediately beneath, sealing them as the soil dries.This is because clay has more total pore space to Subsequent rainfall is much more likely to runhold water, but some of these pores are so small off than to flow into the soil (Figure 1). In con-that the water is held too tightly for plants to trast, a well-aggregated soil resists crusting be-extract. Sand has less total pore space to hold cause the water-stable aggregates are less likelywater, but most of the water it can hold is avail- to break apart when a raindrop hits them. Takeable to plants. Finally, water evaporation from note, however, that any management practicesandy soils is faster than from clay soils. As any that protects the soil from raindrop impact willfarmer knows, sandy soils dry out more quickly decrease crusting and increase water flow intoafter a rain and plants growing on them show the soil. Mulches and cover crops serve this pur-drought signs sooner compared to finer-textured pose well, as do no-till practices which allow thesoils. Consequently, it is wise to put drought- accumulation of surface residue.tolerant crops on the most drought-prone soils,and drought-sensitive crops on finer-textured A soil’s texture and aggregation determine airsoils. and water circulation, erosion resistance, loose- ness, ease of tillage, and root penetration. How- ever, while texture is an innate property of the Table 1. Soil texture’s effects on soil moisture. (1) native soil and does not change with agricultural activities, aggregation can be improved or de- Texture Total Water Available Water Inches/foot Inches/foot stroyed readily through our choice and timing Designation of farm practices. Sand 1.2 0.9 Sandy loam 1.9 1.3 Fine sandly loam 2.5 1.7 Loam 3.2 2.0 Silt loam 3.5 2.1 Sandy clay loam 3.7 2.1 Clay loam 3.8 2.0 Silky clay loam 3.8 1.7 Clay 3.9 1.5AggregationSoil aggregation refers to how the sand, silt, andclay come together to form larger granules. Goodaggregation is apparent in a crumbly soil withwater-stable granules that do not disintegrateeasily. Well-aggregated soil has greater waterentry at the surface, better aeration, and morewater-holding capacity than poorly aggregated Figure 1. Effects of aggregation on watersoil (2). Plant roots occupy a larger volume of and air entry into the soil.well-aggregated soil; better rooting increases thedepth and area plants can reach for water. These Derived from: Land Stewardshipare all positive attributes for drought resistance. Project Monitoring Toolbox (3)PAGE 2 //DROUGHT RESISTANT SOIL
  3. 3. Some practices that destroy or degrade soil ag- Organic Matter and Water-holdinggregates are: Capacity• Excessive tillage Soil holds water according to its texture, as shown• Tilling when the soil is too wet or too dry in Table 1. However, the level of organic matter• Using anhydrous ammonia, which speeds also determines how much water a soil can hold. the decomposition of organic matter• Excessive nitrogen fertilization Arkansas soil scientists report that for every 1%• Excessive sodium buildup from salty irriga- of organic matter content, the soil can hold 16,500 tion water or sodium-containing fertilizers gallons of plant-available water per acre of soil down to one foot deep (5). That is roughly 1.5Aggregation is closely associated with biologi- quarts of water per cubic-foot of soil for eachcal activity and the level of organic matter in the percent of organic matter. Figure 2 shows thesoil. The gluey substances that bind components relationship of organic matter to water-holdinginto aggregates are created largely by the vari- capacity.ous living organisms present in healthy soil.Therefore, aggregation is increased by practicesthat favor soil biota. Because the binding sub- 60stances are themselves susceptible to microbialdegradation, organic matter needs to be replen- 50 % Water by Volumeished to maintain aggregation. To conserve ag-gregates once they are formed, minimize the fac- 40tors that degrade and destroy them. 30The best-aggregated soils are those that havebeen in long-term grass production (4). A grass 20sod extends a mass of fine roots throughout the 10topsoil, contributing to the physical processesthat help form aggregates. Roots continually re- 0move water from soil microsites, providing lo-cal wetting and drying effects that promote ag- 1 2 3 4 5 6 7gregation. Roots also produce food for soil mi- Percent Organic Matter by Weightcroorganisms and earthworms, thus generatingthe compounds that bind the aggregates intowater-stable units. Additionally, a perennial Figure 2. Available water content with increasing soil organic matter (6).grass sod provides protection from raindrops anderosion while these processes are occurring. In addition to holding water, organic matter also improves aggregation. As soil organic matterThis combination of factors creates optimal con- breaks down, large amounts of glues andditions for establishing a well-aggregated soil slimes—the cementing agents of aggregation—under a perennial cover. Conversely, cropping are produced by microbes in the decompositionsequences that involve annual plants in exten- process. A good demonstration of this is pro-sive cultivation provide less vegetative cover and vided in Table 2. The increasing manure rateorganic matter, and usually result in a rapid de- shown in Table 2 led to improved infiltrationcline in soil aggregation and organic matter. No- through the increase in soil aggregation.till cropping requires less manipulation of the soiland retains a surface mulch; it is quite successfulat promoting good aggregation on annually Ground Covercropped soils. The most apparent benefit of maintaining ground cover on soil is erosion resistance. However, //DROUGHT RESISTANT SOIL PAGE 3
  4. 4. Table 2. Water entry into the soil after Table 3. Water evaporation and transpiration *1 hour (2). from tillage types over a 5 month growing season (8). Manure Rate Inches of Water (Tons/acre) Tillage Type Evaporation Transpiration* 0 1.2 No till mm of water mm of water C o v e n t i o n a l 41 307 8 1.9 Till 191 242 16 2.7 *Transpiration is the release of water vapor by plants.ground cover is also associated with drought-proofing. This has been well demonstrated by a importance to drought-proofing, however, is theresearch team at Indiana using variable applica- extent to which a surface cover is maintained.tion of straw. Higher application resulted inhigher water infiltration rates, up to 2.5 tons ofstraw per acre (Figure 3). Table 4. Tillage effects on water infiltration and ground cover (2). Water Infiltration Ground Cover 3 mm/minute Percent 2.5 No till 2.7 48 Chisel Plow 1.3 27Water - inches/hr 2 Moldboard Plow 0.8 12 1.5 1 Table 4 shows three different tillage methods and how they affect water entry into the soil. Notice 0.5 the direct relationship between tillage type, 0 ground cover, and water infiltration. No-till has more than three times the water infiltration of 0 0.25 0.5 1 3 4 moldboard-plowed soil. Additionally, the no- till field would have higher aggregation from the Straw - tons/ac organic matter decomposing on-site. Table 5 shows increases in water infiltration in a dry soilFigure 3. Effect of straw rate on water infiltration on a siltloam soil (7). between no-till and conventional tillage systems; water continues to infiltrate well after the soilSurface cover also reduces water evaporation becomes wet. An often-ignored factor in soilfrom soil. In a Kentucky study, surface evapora- water infiltration is the contribution made bytion was five times less under no-till (which earthworm channels. In soils with high earth-leaves a surface mulch) than with conventional worm populations, 30 to 50 nearly pencil-sizedtillage over the May to September season (Table vertical tunnels per square yard are common (10).3). Because less water was lost to evaporation, Gently sloping land under a mid-summer cornmore water was available for plants. canopy can absorb a 4-inch rainfall in 2 hours with virtually no runoff when abundant earth-Tillage systems and equipment have enormous worm populations are present (10).impacts on water infiltration, storage, and plantefficiency. These include mechanical stress on Gantzer and Blake (11) examined soil channelssoil aggregates, effects on soil microorganisms, created by earthworms and plant roots in a clayand the tendency to create hardpans. Of most loam soil in Minnesota. At the 3 to 6 inch soilPAGE 4 //DROUGHT RESISTANT SOIL
  5. 5. Table 5. Effects of tillage on water (13). A well-structured Indiana soil showed simi-infiltration on a silt loam soil (9). lar total corn root weights under no-till but more Tillage History Dry Soil Wet soil of the roots were in the top 3 inches of soil (14). mm water/hour mm water/hour Table 7. Effect of tillage on ground cover and No-till 43 22 water storage (12). Conventional till 31 10 Tillage System % Ground Cover % Water Storeddepth, the abundance of channels from roots and No-till 78 130worms was approximately three times higher Stubble mulch 38 123under no-till than where the soil was fall plowed(Table 6). Of course with more channels, the rateof water infiltration is higher, resulting in more Deep tillage encourages deep rooting; subsoilingwater capture from each rainfall. can increase rooting depth and impart increased drought protection. Before subsoiling, determine whether it is necessary. Push a sharpened steelTable 6. Soil earthworm and plant root probe in the ground to test for compaction. Ifchannels at the 3 to 6 inch depth during two you are going to be planting on the same rowsseasons, under two tillage regimes (11). year after year (as with ridge-till), probe on top of the rows. Season No-till Fall plow Channels/m2 Channels/m2 Additionally, you can dig a 2-foot-deep hole and Spring 1317 420 run a knife blade through the sidewall of the hole Fall 635 216 to check for resistance. Where the knife blade stops is where the hardpan is. When adjusting the depth of the subsoiler shank, you will wantThe data in Table 7 point out that increased to run it just under the compacted layer. For ex-ground cover enhances water storage as well as ample, if the bottom of the layer is 9 inches deep,infiltration. The surface mulch typical of no-till then run the shank at 10 or 11 inches, not 12 orfields acts as a protective skin to the soil, reduc- 13. Running as shallow as necessary will reduceing the impact of raindrops, buffering the soil draft requirements and cost. Subsoiling shanksfrom temperature extremes, and reducing water can also be run in-row, leaving the surface largelyevaporation. undisturbed. The in-row surface layer must be firmed up to prevent the seed from falling deepTillage also affects plant rooting, and thereby into the subsoil cracks, however. This is typi-directly affects the efficiency of water withdrawal cally done with attachments on the planter.by crop plants. Because it prunes roots and driesthe soil surface, row-crop cultivation discourages No-till and reduced-tillage systems benefit soil.shallow rooting. No-till, in contrast, encourages The advantages of a no-till system include supe-an abundance of roots near the soil surface. Since rior soil conservation, moisture conservation,water infiltration and storage are higher under reduced water runoff, long-term buildup of or-no-till, plant roots find the water and nutrients ganic matter, and increased water infiltration. Athey need closer to the surface. soil managed without tillage relies on soil organ- isms to take over the job of plant-residue incor-In some no-till situations, total root volume is less poration formerly done by tillage. On the downthan in plowed soils. One study showed 34% side, no-till can foster a reliance on herbicides tofewer corn roots at the 2-foot depth under no-till control weeds and can lead to soil compaction //DROUGHT RESISTANT SOIL PAGE 5
  6. 6. from the traffic of heavy equipment. Pioneering Meadow Farm. He has a video showing how hedevelopment work on low-chemical no-till farm- manages his cover crops and plants into them:ing is proceeding at several research stations inthe eastern U.S. and on at least one farm. No-till Vegetables by Steve Groff. 1997. 35 min- utes.Farmer Profiles This video leads the viewer from selection of the proper cover crop mix to plant into, to how to con-In reviewing many articles for this publication, I trol cover crops with little or no herbicide usingsaw numerous farmer testimonials for increased mechanical cover-crop-kill methods, to no-tilldrought tolerance and higher water capacity transplanting of vegetables. Includes commentsfrom no-till. Here are three examples: from leading researchers in no-till vegetable pro- duction. Available for $21.95 + $3.00 shipping•Georgia coastal plain farmer Lamar Black ap- from:plied irrigation water at a rate of 1.5 inches per Cedar Meadow Farmhour on his 1993 corn crop that had been con- 679 Hilldale Roadverted to no-till. The year before, that same field Holtwood, PA 17532would only take in ½ inch of irrigation water per 717-284-5152hour—a higher rate produced runoff (15). http://www.cedarmeadowfarm.com (This website provides lots of good infor-•David Iles of North Carolina says his silage mation and photos of no-till in action.)yields averaged 12 to 15 tons per acre with ad-equate rainfall and 4 to 5 tons without it before Summaryswitching to no-till. After no-till, he makes 20tons per acre with adequate rainfall and 10 tons High aggregation, abundant surface crop resi-without enough rainfall. David says that water due, and a biologically active soil are keys tois his limiting factor. If he gets rain he will make drought-proofing a soil. All these qualities aretop yields, since switching to no-till. He realizes advanced by reduced-tillage systems. In short,that organic matter is the engine that drives his maintaining high residue and adding organicsystem and provides food for earthworms and matter while minimizing or eliminating tillagemicroorganisms. David Iles built his soil by fal- promotes maximum water conservation.lowing out 20 to 25 acres of his 380-acre farm eachyear. On these fallow acres he spreads manure Referencesand then sows crops that are not harvested butgrown as a green manure for their organic mat- 1) Rahn, J. J. 1979. Making the Weather Workter. Even weeds are not clipped but left for their for You. A Practical Guide for Gardener andorganic matter. David loves his earthworms and Farmer. Garden Way Publishing, Charlotte,says they are the best employees he has. “They Vermont. 204 p.work all the time and eat dirt for a living” (16). 2) Boyle, M., W.T. Frankenberger, Jr., and L.H.•Pennsylvania farmer Steve Groff has been farm- Stolzy. 1989. The influence of organic mat-ing no-till with minimal herbicides and exten- ter on soil aggregation and water infiltration.sive use of cover crops for 15 years in Lancaster Journal of Production Agriculture. Vol. 2.County, Pennsylvania. In the spring he rolls the p. 209–299.cover crops down using a 10-foot rolling stalkchopper, which kills the rye or vetch and creates 3) Land Stewardship Project. 1998. The Moni-a nice no-till mulch into which he plants a vari- toring Toolbox. White Bear Lake, MN. Pageety of vegetables and grain crops. After several number unknown.years of no-till production, his soils are mellowand easy to plant into. Steve farms 175 acres of 4) Allison, F.E. 1968. Soil aggregation—somevegetables, alfalfa, and grain crops on his Cedar facts and fallacies as seen by a microbiolo- gist. Soil Science. Vol. 106, No. 2. p. 136–143.PAGE 6 //DROUGHT RESISTANT SOIL
  7. 7. 5) Scott, H.D., L.S. Wood, and W.M. Miley. 14) Cruz, J. C. 1982. Effect of crop rotation and 1986. Long-term effects of tillage on the re- tillage systems on some soil physical proper- tention and transport of soil water. Arkan- ties, root distribution, and crop production. sas Water Resources Research Center. Pub- Ph.D. thesis, Purdue, University, West lication Number 125. 39 p. Lafayette, IN.6) Hudson, B. E. 1994. Soil organic matter and 15) LaRose, J., and J. Dirnberger. 1996. The little available water capacity. Journal of Soil and pluses add up. National Conservation Till- Water Conservation. Vol. 49, No. 2. p. 189– age Digest. Fall. p. 5–7. 194. 16) Dirnburger, J.M., and M. LaRose. 1997. No-7) Mannering, J.V., and L.D. Meyer. 1963. The till saves dairy farm by healing the harm that effects of various rates of surface mulch on tillage has done. National Conservation Till- infiltration and erosion. Soil Science Society age Digest. Summer. p. 5–8. of America Proceedings. Vol. 27. p. 84–86.8) Phillips, R.E. 1980. Soil Moisture. In: R.E. Phillips, G.W. Thomas, and R.L. Blevens (eds.) By Preston Sullivan No Tillage Research: Research Reports and NCAT Agriculture Specialist Reviews, University of Kentucky, College of Agriculture and Agriculture Experiment Sta- Edited by Richard Earles tion, Lexington. p. 23–42. Formatted by Cynthia Arnold9) McGregor, K.C., C.K. Mutchler, and R.F. November 2002 Cullum. 1991. Soil erosion effects on soy- bean yield. Paper N. 912626. American So- ciety of Agricultural Engineers, St. Joseph, MO.10) Staff. 1993. Land’s best friend. In: Pro- The electronic version of Drought Resistant Soils is located at: ceedings: National No-tillage Confer- HTML ence, 1993, Cedar Falls, IA. p. 317–320. http://www.attra.ncat.org/attra-pub/drought.html [Reprinted from LandOwner.] PDF http://www.attra.ncat.org/attra-pub/PDF/drought.pdf11) Gantzer, C.J., and G.R. Blake. 1978. Physical characteristics of Le Sueur clay loam soil fol- IP169 lowing no-till and conventional tillage. Agronomy Journal. Vol. 70. p. 853–857.12) Peterson, G.A., and C.R. Fenster. 1982. No- till in the great plains. Crops and Soils Maga- zine. Vol. 43. p. 7–9.13) Navas, A.J. 1969. The effect of several till- age systems on some soil physical properties and on corn growth. MS Thesis, Purdue Uni- versity. August, Catalog number 22652, West Lafayette, IN. //DROUGHT RESISTANT SOIL PAGE 7