Abstract

In order to examine the nutrient content, and the distribution and accumulation patterns of individual nutrients in the natural secondary forests (NSFs), sample NSF plots were selected in the Caijiachuan watershed on the Loess Plateau. On the basis of a comprehensive field inventory to the NSFs in Caijiachuan watershed, a 40 m × 40 m sample plot was selected as the representative plot. Each tree plant was then measured to select the standard tree in accordance with a diameter-scale. For measurement of the biomass in the above-ground part of the tree, it was divided into parts and measured. The study measured the concentration of the 5 major macronutrients (namely N, P, K, Ca and Mg) and the 8 major micronutrients (namely Cd, Fe, Mn, Cu, Zn, Pb, Ni and B) in plant organs. An appropriate amount of the samples were weighed and exposed to H2SO4-H2O2 using the Kjeldahl heating digestion method. While N content was measured with the semi-micro determination method, P content was measured using vanadium molybdate yellow colorimetric method HNO3-HClO4 ICP heating digestion method was applied to determine the contents of Ca, Mg, K, Na, Fe, Cu, Zn, Mn, B, Cd, Pb, Ni. As for soil samples, corresponding approaches were employed to work out the contents of each of the above-mentioned nutrient elements. Among the tree, shrub and herbaceous layers, the content of macro-nutrients follows the sequence of Ca > N > K > Mg > P, compared with their counterpart of K > N > Ca > P > Mg in the litter layer. For the micronutrient contents, similar sequences (i.e., Fe > Mn > Zn > B > Cu > Pb > Ni > Cd) were observed in the tree, shrub and litter layers; whereas the herbaceous layer demonstrated a different sequence of Fe > Mn > B > Zn > Cu > Pb > Ni > Cd. Within the NSF ecosystem, total accumulation of the 5 major macronutrients (excluding that in the soil) reached 1089.82 kg/ha, of which the tree layer took up the largest share, 40.82%, followed in turn by the shrub layer (31.28%), the herbaceous layer (12.55%) and the litter layer (15.36%). In terms of nutrient-concentration in the plant organs within the tree layer, the overall sequence can be expressed as branches > roots > wood > bark > leaves. The total accumulation of the 5 major macro-nutrient in the soil reached 634.97 t/ha. In terms of the accumulation coefficients in each of the layers, the general pattern can be summed up as: shrub layer > tree layer > herbaceous layer, and N > P > Ca > K > Mg. In terms of the plant organ accumulation coefficients at the tree layer, the sequence was leaves > branches > roots > bark > wood. As for the accumulation coefficients of the micronutrients, the overall sequences for the tree layer, the shrub layer and the herbaceous layer can be listed as Cd > B > Zn > Cu > Mn > Ni > Pb > Fe; Cd > B > Zn > Mn > Cu > Ni >Pb > Fe and Cd > B > Mn > Zn > Cu > Ni > Pb > Fe, respectively. The study also revealed that the macronutrients that are absorbed, assimilated and returned by the NSF stand annually reached 99.054kg/(ha·year), 49.155 kg/(ha·year) and 49.899 kg/(ha·year), respectively, demonstrating a well-balanced state of nutrient cycling. With an average of 0.0013, the absorbance index of the macro-nutrients was ranked in the following sequence, N > P > K > Ca > Mg; whereas their utilization and cycling indexes were respectively sequenced as K > P > N > Mg > Ca and K > P > N > Mg > Ca. For the micronutrients the corresponding annual figures were 117.35 g/(ha·year), 50.96 g/(ha·year) and 66.39 g/(ha·year), respectively. The micronutrients, as a whole, showed a relatively small absorbance index (e.g.,Cd was the largest =0.0036). The average utilization index of all the microelements was 0.12.

Highlights

  • The accumulation and distribution of tree nutrients forms the basis for studying energy and nutrient cycling within forest ecosystems

  • The upper and middle reaches of the Caijiachuan watershed are mainly covered with natural secondary forests (NSFs) that are composed of Populus davidiana, Quercus wutaishabcia Mayr, Betula platyphylla Suk. and Ostryopsis davidiana, with Populus davidiana as the dominant species

  • On the unique landscape on the Loess Plateau, the biomass within the tree layer still makes up the largest share, but that in the vigorousgrowing shrub layer amounts almost to 1/3 of the total

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Summary

Introduction

The accumulation and distribution of tree nutrients forms the basis for studying energy and nutrient cycling within forest ecosystems. Bio-cycling of nutrients, one of the major functions of forest ecosystems, is closely related to carboncycling; it is of great significance in fields such as restoration-ecology, biodiversity and global climate change. A precise estimate of vegetation carbon-storage is becoming a key component in elaborating the role of vegetation restoration in ensuring a balanced carbon content in terrestrial ecosystems; it is critical in examining the relationship between global climate change and carbon cycling (Watson, 2000). Extensive research has been carried out on mineral elements, including N, P, K, Ca, Mg and their corresponding physiological functions that are needed for plant growth in terms of mass. Similar research on trace elements within plants, including their absorbance, transportation within plants, their physiological as well as biochemical functions, their impacts on the growth and quality of plants, and prevention and testing of heavy metal pollution to plants, have yielded promising results (You et al, 2005)

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