
 
        
         
		wastes, and other materials.  
 Peat, aka peat moss, has been a standard organic  
 source. It is still the same good product as in the  
 past, but may occasionally contain weed seeds or  
 pathogens, depending upon method of harvesting.  
 Peat decomposes more slowly than most other organic  
 sources and thus may give its effects comparably longer.  
 Animal manures have for years been among the best  
 organic sources. While providing organic matter they  
 can also be a good source of plant nutrients. Partially  
 decomposed “old manure” is a good source of organic  
 matter but inferior to fresh manure in plant nutrients.  
 The fear of “burning” with fresh manure is easily offset  
 by applying less of the better product. Unfortunately  
 manure may contain numerous weed seeds, including  
 those of noxious weeds.  
 When purchasing manure, inspect carefully  
 for unwanted problems. One, garden centipedes  
 (symphyllans) introduced into a soil can cause  
 tremendous damage for years to come by feeding on  
 plant roots. It’s best to avoid manure stored for any  
 length of time on the ground. Older manures are more  
 likely to come with these problems.  
 Organic materials high in lignin, such as wood  
 products, straw, grass hay, and hulls, can deplete soil  
 nitrogen during their decomposition. Supplemented  
 nitrogen, supplied by a fertilizer relatively high in  
 nitrogen, will correct the deficiency. Wood products  
 take up to four years of decomposition for the  
 “softwoods”—pine, fir, spruce, etc.—before a nitrogen  
 balance is reached in the soil. Hardwoods—oak, maple,  
 beech, etc.—take about half this amount of time for  
 decomposition. This is usually not a problem with  
 peat since it naturally contains some nitrogen, or with  
 composts, leaf mold, manures, and other such sources. 
 Dealing With Sandy Soils 
 A truly sandy soil will feel gritty when rubbed  
 between the fingers. Most sandy soils have at least a  
 little clay and silt in them, but insufficient amounts of  
 clay, especially to hold nutrients and water. Structure of  
 sandy soils may be either loose or, with an insufficient or  
 “wrong” amount of smaller particles and organic matter,  
 hard and crusty and impenetrable to water when dry.  
 They are inherently low in plant nutrients and good tilth.  
 Sandy soils can be much improved by “diluting” with  
 good soil and/or organic matter. The amendment(s)  
 should be thoroughly worked into the top six or more  
 inches of the soil, as deeply as possible.  
 It is wrong to assume that a sandy soil is well drained.  
 If the sand is underlaid by a compacted layer, drainage  
 can be a serious problem.  
 Generally, in sandy soils fertilizer should be applied  
 in lesser amounts but more frequently to avoid loss by  
 leaching and contaminating ground water. This is more  
 important with water-soluble inorganic than with organic  
 fertilizers. 
 Soil Testing 
 Testing your soil is a good way to determine the  
 pH (acidity or alkalinity), need for pH correction,  
 and nutrient content of your soil, with suggestions. A  
 good soil sample for testing is a composite of samples  
 taken throughout your garden, then thoroughly mixed  
 together when sufficiently dry by pouring back and forth  
 from one clean bucket to another. Follow all instructions  
 of the testing laboratory to which you will submit your  
 soil sample. One thing you will not learn about your soil  
 from the test is the soil’s texture; that is, if it is a clay,  
 clay loam, loam, etc. A few labs, however, can make a  
 texture test for you for an additional fee. 
 Generally Speaking 
 Organic matter will do as much, or more, to improve a  
 given soil than most any other practice. Worked deeply  
 into the soil, its effects can often be seen for years to  
 follow. The only real “downside” in using organic matter  
 is the nitrogen imbalance that high lignin materials can  
 present, and the potential for insect, weed, and disease  
 problems of some organic sources. Seldom do the  
 problems outweigh the benefits. 
 Keep in mind that working a soil when it is excessively  
 wet or when excessively dry should be avoided. When  
 too wet the soil structure is broken down, causing  
 puddling or “plastic remolding.” When too dry, the  
 soil is ground or pulverized into dust, also causing a  
 breakdown of structure. In between lies a rather narrow  
 range of wetness for optimal cultivation of the soil. 
 Improve your soil—make it enjoyable and watch your  
 garden grow! 
 d 
 Fall 2018 AIS Bulletin 47