forest soil fertility studies

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FOREST SOIL FERTILITY STUDIES by W. L. POWERS and W. B. BOLLEN, Oregon Agricultural Experiment Station. Chemical Characteristics In a chemical study made of DeKalb and Upshaw forest soil profiles from Pennsylvania and of Olympic and Aiken soil profiles from the Oregon State College, or "Peavy Arboretum", it appears (1) that the organic matter extends deeper in the western Oregon profiles and nitrogen carries down with it the maximum nitrogen content in each of the forest soil profiles is approximate- ly at the F-H boundary zone. (2) Base exchange capacity also reaches a maximum at about this zone, where the major part of the colloidal material is organic and in- timately mixed with minor amount of inorganic soil col- loids. (3) DeKalb soil seems more aged and lower in base exchange capacity than the others. Nitrate Supplying Power A study made of nitrate supplying power of organic materials from two Oregon soil profiles made by adding sufficient material from each horizon to supply one and one-half grams of nitrogen in 3800 grams of quartz sand, using growth of oats as an indicator, indicates maximum nitrogen supplying power in the H or HS layer as judged by dry matter yield and nitrogen con- tent therein. A parallel series of fallow jars similarly prepared and leached each two weeks for two months yielded similar relative amounts of nitrate. Liming appears to have increased the yield of nitrate slightly. Fertilizer Requirements Of Forest Soils Nitrate need of fir seedlings grown on Aiken silty clay loam was further tested in beds 100 by 25 by 25 centimeters on each of which 21 year fir seedlings wer^ grown. Two checks and nine treatments were included. Sodium nitrate was added at rates of 8, 16, 32, 64, 128, and 256 p.p.m. nitrogen, also 32 p.p.m. in the forms of ammonium surfate, bloodmeal and forest litter. Increase in diameter, height and weight of Douglas fir seedlings indicate 64 p.p.m. nitrogen gave maximum growth. The heaviest app'ication was excessive. Organic forms of nitrogen appear very suitable. A pupil, H. J. Stewart, cooperated in this test. In a triangle fertilizer experiment with holly seed- lings, potassium sulfate yielded a maximum increase in height on Newberg fine sandy loam. Mr. Robert Brown, a student, cooperated in this experiment. A fertilizer experiment with Douglas fir seedlings conducted on Olympic silty clay loam at the College Ar- boretum nursery in 1932 and 1933 indicates that well decayed nitrogenous organic matter, or conifer litter and nitrate are more effective in inducing growth than chemicals supplying phosphorus and potassium. Microbial Characteristics Numbers of bacteria, actinomycetes, and molds were most abundant in the F and H layers, generally being slightly more numerous in the former. DeKalb horizons gave unusual results in that molds exceeded bacteria in both F and H horizons and actino- mycetes were found only in the litter. The Olympic serives gave much higher counts of bacteria and actino- mycetes than did Aiken horizons, although the numbers of molds were similar in both. In general, bacteria were twice as numerous as actinomycetes while molds, as determined separately on an acid medium, made up from one to five per cent of the total. Page 24

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Page 1: Forest Soil Fertility Studies

FOREST SOIL FERTILITY STUDIESby

W. L. POWERS and W. B. BOLLEN,Oregon Agricultural Experiment Station.

Chemical Characteristics

In a chemical study made of DeKalb and Upshawforest soil profiles from Pennsylvania and of Olympicand Aiken soil profiles from the Oregon State College,or "Peavy Arboretum", it appears (1) that the organicmatter extends deeper in the western Oregon profilesand nitrogen carries down with it the maximum nitrogencontent in each of the forest soil profiles is approximate-ly at the F-H boundary zone. (2) Base exchange capacityalso reaches a maximum at about this zone, where themajor part of the colloidal material is organic and in-timately mixed with minor amount of inorganic soil col-loids. (3) DeKalb soil seems more aged and lower in baseexchange capacity than the others.

Nitrate Supplying Power

A study made of nitrate supplying power of organicmaterials from two Oregon soil profiles made by addingsufficient material from each horizon to supply oneand one-half grams of nitrogen in 3800 grams of quartzsand, using growth of oats as an indicator, indicatesmaximum nitrogen supplying power in the H or HSlayer as judged by dry matter yield and nitrogen con-tent therein.

A parallel series of fallow jars similarly preparedand leached each two weeks for two months yieldedsimilar relative amounts of nitrate. Liming appears tohave increased the yield of nitrate slightly.

Fertilizer Requirements Of Forest Soils

Nitrate need of fir seedlings grown on Aiken siltyclay loam was further tested in beds 100 by 25 by 25centimeters on each of which 21 year fir seedlings wer^

grown. Two checks and nine treatments were included.Sodium nitrate was added at rates of 8, 16, 32, 64, 128,and 256 p.p.m. nitrogen, also 32 p.p.m. in the forms ofammonium surfate, bloodmeal and forest litter. Increasein diameter, height and weight of Douglas fir seedlingsindicate 64 p.p.m. nitrogen gave maximum growth. Theheaviest app'ication was excessive. Organic forms ofnitrogen appear very suitable. A pupil, H. J. Stewart,cooperated in this test.

In a triangle fertilizer experiment with holly seed-lings, potassium sulfate yielded a maximum increase inheight on Newberg fine sandy loam. Mr. Robert Brown,a student, cooperated in this experiment.

A fertilizer experiment with Douglas fir seedlingsconducted on Olympic silty clay loam at the College Ar-boretum nursery in 1932 and 1933 indicates that welldecayed nitrogenous organic matter, or conifer litterand nitrate are more effective in inducing growth thanchemicals supplying phosphorus and potassium.

Microbial Characteristics

Numbers of bacteria, actinomycetes, and molds weremost abundant in the F and H layers, generally beingslightly more numerous in the former.

DeKalb horizons gave unusual results in that moldsexceeded bacteria in both F and H horizons and actino-mycetes were found only in the litter. The Olympicserives gave much higher counts of bacteria and actino-mycetes than did Aiken horizons, although the numbersof molds were similar in both. In general, bacteria weretwice as numerous as actinomycetes while molds, asdetermined separately on an acid medium, made up fromone to five per cent of the total.

Page 24