1960Unpublished venueRequires access

Solubility Curves of Inorganic Phosphorus in the Paddy Soils of Taiwan

Hsieng‐Cheng Tseng

Open publisher page 1 citations

Abstract

The pH-solubility curve of inorganic soil phosphorus of the main soil groups of Taiwan was summarized as follows: (1) In the acid red earth or yellow earth and mudstone alluvial soil, iron and aluminum phosphate may be the principal form of phosphorus. (2) In the slate alluvial soils, schist alluvial soils and saline alluvial soils, calcium phosphate is predominent form of inorganic soil phosphorus. (3) In the sandstone and shale alluvial soils, both calcium phosphate and iron, aluminum phosphates are present in about equal amount. (4) The minimum solubility of phosphorus in the soils of different soil groups are generally in the pH range of 6 to 8.

About this research paper

What this paper is about

The pH-solubility curve of inorganic soil phosphorus of the main soil groups of Taiwan was summarized as follows: (1) In the acid red earth or yellow earth and mudstone alluvial soil, iron and aluminum phosphate may be the principal form of phosphorus. (2) In the slate alluvial soils, schist alluvial soils and saline alluvial soils, calcium phosphate is predominent form of inorganic soil phosphorus. (3) In the sandstone and shale alluvial soils, both calcium phosphate and iron, aluminum phosphates are present in about equal amount. (4) The minimum solubility of phosphorus in the soils of different soil groups are generally in the pH range of 6 to 8.

Why it matters

OpenAlex reports 1 citations for this work. Citation counts describe recorded attention and do not establish research quality.

Key contribution

A contribution statement is not available in the OpenAlex record.

Method / approach

Method details are not available in the OpenAlex metadata.

Main findings

Findings are not separately available in the OpenAlex metadata.

Limitations

Limitations are not available in the OpenAlex metadata.

Applications

Application details are not available in the OpenAlex metadata.

Available abstract

The pH-solubility curve of inorganic soil phosphorus of the main soil groups of Taiwan was summarized as follows: (1) In the acid red earth or yellow earth and mudstone alluvial soil, iron and aluminum phosphate may be the principal form of phosphorus. (2) In the slate alluvial soils, schist alluvial soils and saline alluvial soils, calcium phosphate is predominent form of inorganic soil phosphorus. (3) In the sandstone and shale alluvial soils, both calcium phosphate and iron, aluminum phosphates are present in about equal amount. (4) The minimum solubility of phosphorus in the soils of different soil groups are generally in the pH range of 6 to 8.

Key concepts: Soil water, Alluvium, Phosphorus, Solubility, Phosphate, Chemistry, Soil pH, Calcium

Related papers

Back to paper searchBrowse research topicsOriginal source
Solubility Curves of Inorganic Phosphorus in the Paddy Soils of Taiwan — Research Paper | ScholarLens