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Introduction.Definition of terms. The nutrient-uptake estimates calculated. The nature and validity of the original data. How the estimates were calculated. The validity of the estimates. The silvicultural significance of the mean estimates. Further aspects of the estimates, causes of variability and comparison with agriculture. The nutrient-uptakes in relation to nutrient-poor soils. Conclusions. Acknowledgements. Literature cited. ABSTRACTThe extremely low nutrient-status of various recently afforested moor soils, particularly Yorkshire (England) Calluna soils, raised the question of their ability to provide the possible nutrient-demands of continuous forest growth. This paper describes how, for calcium, potassium and phosphorus, uptake estimates have been calculated from existing nutrient-composition data, and discusses the silvicultural significance of such estimates, particularly in relation to nutrient-poor soils.All existing nutrient-composition data for whole individual mature temperate forest trees are summarized: using yield-data and a method of calculation critically discussed, they are made to provide nutrient-uptake estimates for one acre of such forest after periods of 50 and 100 years' growth. Mean estimates representing "hard~vood," "other conifer" and "pine" forest are then calculated showing : --the nutrients removed from the site via the various components of the timber-thinnings and clear-fellings, the --4 9 -- Plant and Soii VII PETER J. RENNIEnutrients taken up and immobilized within the various component organs of the growing forest, and the total nutrient-uptake from the site. The estimates show that timber exploited forest, by reason of its unavoidable continuous nutrient-removal from the site, differs fundamentally from unexploited virgin forest; in absolute terms this removal may be small, but its pedologicaI and silvicultural importance upon any particular site, depends entirely upor~ the ability of the soil to replenish this loss. It is believed that up to now the failure to recognize this nutrient-removal upon nutrient-poor soils has diverted attention from an important factor initiating both soil-degradation and diminishing site-productivity.Soil nutrient-data presented show that the nutrient-uptakes of timberproducing forest of either coniferous or hardwood species are so large compared with the nutrient-contents of moor soils that further overall soil-degradation and, sooner or later, diminished site-productivity are inevitable.Upon such soils, therefore, continuous timber production cannot be sustained by ploughing or by the growth of hardwoods alone; new silvicultural techniques are needed which can restore to the site, by means of suitable soil-ameliorants and methods yet to be evolved, the nutrients continually being removed via the timber.The paucity of knowledge concerning both the nutrient-demands of common tree species and the nutrient-status of the nutrient-poor soils upon which they are being extensively planted calls for an expansion of research upon these aspects if ti...
Introduction.Definition of terms. The nutrient-uptake estimates calculated. The nature and validity of the original data. How the estimates were calculated. The validity of the estimates. The silvicultural significance of the mean estimates. Further aspects of the estimates, causes of variability and comparison with agriculture. The nutrient-uptakes in relation to nutrient-poor soils. Conclusions. Acknowledgements. Literature cited. ABSTRACTThe extremely low nutrient-status of various recently afforested moor soils, particularly Yorkshire (England) Calluna soils, raised the question of their ability to provide the possible nutrient-demands of continuous forest growth. This paper describes how, for calcium, potassium and phosphorus, uptake estimates have been calculated from existing nutrient-composition data, and discusses the silvicultural significance of such estimates, particularly in relation to nutrient-poor soils.All existing nutrient-composition data for whole individual mature temperate forest trees are summarized: using yield-data and a method of calculation critically discussed, they are made to provide nutrient-uptake estimates for one acre of such forest after periods of 50 and 100 years' growth. Mean estimates representing "hard~vood," "other conifer" and "pine" forest are then calculated showing : --the nutrients removed from the site via the various components of the timber-thinnings and clear-fellings, the --4 9 -- Plant and Soii VII PETER J. RENNIEnutrients taken up and immobilized within the various component organs of the growing forest, and the total nutrient-uptake from the site. The estimates show that timber exploited forest, by reason of its unavoidable continuous nutrient-removal from the site, differs fundamentally from unexploited virgin forest; in absolute terms this removal may be small, but its pedologicaI and silvicultural importance upon any particular site, depends entirely upor~ the ability of the soil to replenish this loss. It is believed that up to now the failure to recognize this nutrient-removal upon nutrient-poor soils has diverted attention from an important factor initiating both soil-degradation and diminishing site-productivity.Soil nutrient-data presented show that the nutrient-uptakes of timberproducing forest of either coniferous or hardwood species are so large compared with the nutrient-contents of moor soils that further overall soil-degradation and, sooner or later, diminished site-productivity are inevitable.Upon such soils, therefore, continuous timber production cannot be sustained by ploughing or by the growth of hardwoods alone; new silvicultural techniques are needed which can restore to the site, by means of suitable soil-ameliorants and methods yet to be evolved, the nutrients continually being removed via the timber.The paucity of knowledge concerning both the nutrient-demands of common tree species and the nutrient-status of the nutrient-poor soils upon which they are being extensively planted calls for an expansion of research upon these aspects if ti...
The parent material of the soil is one of the most important factors influencing soil development. Where the soil develops on rock the classification of the parent material is relatively straightforward, but in countries such as Britain where widespread glaciation has occurred and the arable soils are mainly developed on glacial drifts, the problem is more complicated. If these drifts are thin and due to a single glaciation there is a close correspondence between them and the underlying rock; but in certain areas, of which north-east Scotland is one, the soil parent materials are complex because of several glaciations and the occurrence of mixed drifts. The mineralogical composition of these drifts in eastern Kincardineshire has been described in Part I of this paper. The area was selected because it provides a good example of diverse rock types of widespread occurrence which have been subjected to three main glaciations. In the present contribution the drifts are discussed in relation to the resulting soil parent materials.The region is relatively low-lying, the highest point being about 1000 ft. There is a flat or gently undulating stretch along the coast, and in the northern district this is succeeded inland by hummocky ground with rocky knolls and depressions generally filled with peat. In the southern district the inland country is diversified by a range of hills running parallel to the coast and succeeded farther inland by a plain which is the northern part of a broad valley called the Howe of the Mearns.
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