Abstract

The Yarlung Zangbo River basin ecosystem is fragile. The distribution and transportation of phosphorus is of great significance for aquatic environmental protection and ecological security. The sequential extraction method and molybdenum antimony anti-spectrophotometry were used to measure the concentrations of different forms of phosphorus in the surface sediments from 15 sampling sites along the middle reaches of the Yarlung Zangbo River and its tributaries. The results show that the total phosphorus concentration in the surface sediments is 194.0~540.7 mg/kg, which is mainly composed of inorganic phosphorus. The concentrations of various phosphorus forms ranked as calcium-bound phosphorus (355.6 ± 86.0 mg/kg) > soluble phosphorus (15.9 ± 10.0 mg/kg) > iron-bound phosphorus (12.4 ± 12.3 mg/kg) > organic phosphorus (9.6 ± 6.1 mg/kg) > occluded phosphorus (9.2 ± 3.8 mg/kg) > aluminum-bound phosphorus (5.4 ± 2.3 mg/kg). On the whole, phosphorus concentration is greater in wet season than dry season. Regarding the spatial distribution characteristics, there are great disparities in the different forms of phosphorus in the middle reaches of the Yarlung Zangbo River. Comprehensive analysis shows that phosphorus of this area is mainly self-generated, and concentration of bioavailable phosphorus is small, demonstrating there will not be a large release. We also drew a “specific triangle” of the different forms of phosphorus concentrations in the research area and defined the “α” angle to determine the nutrient status of the overlying water quickly and effectively. Finally, phosphorus flux of the mainstream was estimated. This research may provide information on the phosphorus of Plateau Rivers.

Highlights

  • Phosphorus is an important biogenic material in nature

  • The results show that there phosphorus concentration of thethe water

  • Forms of P in the YLZB River basin were classified as Ca-P, SP, Fe-P, OP, Oc-P, and Al-P

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Summary

Introduction

Phosphorus is an important biogenic material in nature. It usually exists in water bodies and sediments in different forms. P usually exists in water, suspended sediments, and sediments settled on river banks [1,2]. The adsorption and desorption processes of different forms of P between overlying water and sediments represent important patterns for P migration and transformation in aquatic ecosystems [3,4]. The analysis of different forms of P in water bodies and sediments is the premise and basis for studying these processes. It is of great significance for aquatic environmental protection and ecological safety

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