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Full-Text Articles in Agriculture

Land Transfers In Twelve Counties In Nebraska, 1928-1933, L. F. Garey Nov 1938

Land Transfers In Twelve Counties In Nebraska, 1928-1933, L. F. Garey

Historical Research Bulletins of the Nebraska Agricultural Experiment Station

The land transfers in twelve counties in Nebraska for the period 1928 to 1933 have been studied and the findings are submitted in this bulletin. The data on which the study is based were obtained from records in the office of the Register of Deeds in each county and from other sources and include transfers which occurred during the period indicated. The counties included in the study are Boone, Cass, Cuming, Dakota, Dawes, Frontier, Gage, Hamilton, Harlan, Lancaster, Nuckolls, and Valley.


The Tax System Of Nebraska With Special Reference To Its Relation To Agriculture, L. B. Snyder Oct 1938

The Tax System Of Nebraska With Special Reference To Its Relation To Agriculture, L. B. Snyder

Historical Research Bulletins of the Nebraska Agricultural Experiment Station

Progress in governmental affairs calls for constant study of matters pertaining to government. The recent agitation for moratoria on debts and taxes and the many tax reforms suggested are evidence of the need for such study. Before satisfactory reforms can be made, information on receipts and expenditures by governmental agencies must be secured. The expense connected with collecting, tabulating, and analyzing such data has prevented private agencies of the state from doing this. Because it was felt that such information would be useful and could be obtained by the College of Agriculture, this study was undertaken.


A Proposed Method For Classifying And Evaluating Soils On The Basis Of Productivity And Use Suitabilities, Arthur Anderson, A. P. Nelson, F. A. Hayes, I. D. Wood May 1938

A Proposed Method For Classifying And Evaluating Soils On The Basis Of Productivity And Use Suitabilities, Arthur Anderson, A. P. Nelson, F. A. Hayes, I. D. Wood

Historical Research Bulletins of the Nebraska Agricultural Experiment Station

It is the object of this paper to present a method for classifying and evaluating the soils as mapped in regular soil surveys on the basis of land types, which are here defined as areas having reasonably similar productivity and use suitabilities. The standards used to differentiate land types will vary according to the desired objectives, but any material difference in yield, or in practices necessary to maintain a desirable level of productivity will justify recognition of land types. The proposed procedure involves a more detailed study of the influence which soils, slope, erosion, and drainage have on specific crops …


Ec38-118 Soil And Moisture Conservation In Nebraska, D.L. J. Gross, E.H. Doll Jan 1938

Ec38-118 Soil And Moisture Conservation In Nebraska, D.L. J. Gross, E.H. Doll

University of Nebraska-Lincoln Extension: Historical Materials

When the white men first explored Nebraska, they found little erosion taking place. They found the hills, particularly in eastern Nebraska, covered with a dense growth of grass, underlain with a thick mat of decaying debris. The valleys were even more densely covered with the water-loving grasses and sedges. The soil underneath the prairie was black and spongy, the result of centuries of accumulating humus. The valleys bordering the streams were boggy and abounded with springs. Clear water flowed constantly in the streams. The upland draws in the more favorable parts of the state were heavily covered with the big …


Ec38-118 Soil And Moisture Conservation In Nebraska, D.L. Gross, E.H. Doll Jan 1938

Ec38-118 Soil And Moisture Conservation In Nebraska, D.L. Gross, E.H. Doll

University of Nebraska-Lincoln Extension: Historical Materials

When the white men first explored Nebraska, they found little erosion taking place. They found the hills, particularly in eastern Nebraska, covered with a dense growth of grass, underlain with a thick mat of decaying debris. The valleys were even more densely covered with the water-loving grasses and sedges. The soil underneath and prairie was black and soggy, the result of centuries of accumulating humus. The valleys bordernig the streams were boggy and abounded with springs. Clear water flowed constantly in the streams. The upland draws in the more favorable parts of the state were heavily covered with the big …