Soil Chemical Properties and Plant Nutrient Status as Influenced by Application of Lime, Phosphorus and Compost

2017 ◽  
Vol 20 (2) ◽  
pp. 1-11
Author(s):  
Dereje Shanka ◽  
Nigussie Dechassa ◽  
Eyasu Elias ◽  
Setegn Gebeyehu
Keyword(s):  
Chemical Properties ◽  
Nutrient Status ◽  
Soil Chemical Properties ◽  
Plant Nutrient

scholarly journals The relationship Between Soil Chemical Properties and Uptake of Tea Plant Nutrient in PTPN VI Jambi

2022 ◽  
Vol 9 (1) ◽  
pp. 181-191
Author(s):  
Arini Ayu Ardianti ◽  
Faris Nur Fauzi Athallah ◽  
Restu Wulansari ◽  
Kurniawan Sigit Wicaksono
Keyword(s):  
Nutrient Uptake ◽  
Soil Ph ◽  
Chemical Properties ◽  
Soil Nutrient ◽  
Tea Plant ◽  
Soil Chemical Properties ◽  
Plant Nutrient ◽  
Plant Nutrient Uptake ◽  
Tea Plants ◽  
The Relationship

Healthy soil could support plant growth by optimizing the availability of nutrients. The availability of nutrients influences the health of tea plants. Nutrient deficiencies would affect the plant physiology that exhibits the plant withering. This study aimed to define the relationship between soil nutrient availability with plant nutrient uptake. This research was conducted by managing secondary data soil chemical properties, and tea plant nutrients analyzed statistically with Pearson correlation. This study only found a significant correlation between soil pH with P and Mg uptake. Correlation results between soil nutrient and plant nutrient uptake obtained a significantly negative correlation on soil pH with P and Mg nutrients with a correlation value of pH-P (r=-0.52), pH-Mg (r=-0.52). There was no correlation between other soil nutrients and plant nutrient uptake. The results of this study can be used to determine the dose of fertilization and the management recommendation of tea plants.

scholarly journals Interactions between leaf macronutrients, micronutrients and soil properties in pistachio (Pistacia vera L.) orchards

2013 ◽  
Vol 72 (2) ◽  
pp. 295-310 ◽  
Author(s):  
Prodromos Koukoulakis ◽  
Christos Chatzissavvidis ◽  
Aristotelis Papadopoulos ◽  
Dimitrios Pontikis
Keyword(s):  
Dry Matter ◽  
Chemical Properties ◽  
Nutrient Status ◽  
Soil Chemical Properties ◽  
Leaf Analysis ◽  
Promote Plant Growth ◽  
Macro And Micronutrients ◽  
Almost All ◽  
Plant Available P ◽  
Pistachio Trees

Abstract - The interactions between: (i) leaf dry matter macronutrietns, micronutrients and soil chemical properties, (ii) leaf macro- and micronutrients, (iii) soil macro- and micronutrients and (iv) soil chemical properties, and soil micro- and macronutrients in 50 pistachio orchards were investigated in leaves and soils by means of regression analysis. Most of the soils were deficient in plant-available P, Zn, Mn, Fe, and B, while they were excessively supplied with Cu. Leaf analysis showed that most of the trees were sufficient in K, Mg, Mn and B, but deficient in N, P and Fe, and excessive in Zn and Cu. It was found that almost all the significant elemental interactions occurring in pistachio leaves or soils were synergistic, contributing considerable quantities of available nutrients and, therefore, improving the nutrient status of pistachio trees, and the level of soil fertility. On the other hand, the interactions between K and Mg in leaves, and between soil pH and leaf N or soil Fe, Mn and B, were antagonistic. It is suggested that these results must be taken into account during fertilization of pistachio trees, in order to avoid nutritional disorders and to promote plant growth, productivity and nut quality.

Studies on some deep sandy soils in Cape York Peninsula, North Queensland. 1. Morphological and chemical characteristics

1973 ◽  
Vol 13 (60) ◽  
pp. 81 ◽  
Author(s):  
RF Isbell ◽  
GP Gillman
Keyword(s):  
Chemical Properties ◽  
Sandy Soils ◽  
Nutrient Status ◽  
Exchangeable Cations ◽  
Soil Sampling ◽  
Granitic Rocks ◽  
Chemical Characteristics ◽  
Plant Nutrient ◽  
Copper Zinc ◽  
Cape York

Deep sandy soils overlying granitic rocks are widespread in Cape York Peninsula. Rainfall is summer dominant and the annual mean is 1140 mm. Evidence is presented that some of the soils are weakly podzolised and some soil properties are influenced by an underlying clay horizon at depth. The method of soil sampling adopted permits a statistical estimate of the variability of soil chemical properties. Most data for the surface soils of this group have a sufficiently low variability both within and between sites to allow an assessment of plant nutrient status derived from associated experiments in field and glasshouse to be generally applicable throughout the region. All soils are very low in organic carbon, nitrogen, potassium, sulphur, phosphorus, copper, zinc, and exchangeable cations.

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