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合成肥料对哥达瓦里河颗粒有机物稳定同位素比率的作用。

Role of synthetic fertilizers on stable isotope ratios of particulate organic matter in the Godavari River.

作者信息

Krishna Moturi Srirama, Naidu Sura Appala, Prasad Mamidala Hari Krishna, Subbaiah Chereddy Venkata, Reddy Nalla Purna Chander, Rao Neerukattu Srinivasa

机构信息

CSIR - National Institute of Oceanography, Regional Centre, Visakhapatnam, 530017, India.

ESSO - Indian National Centre for Ocean Information Services, Hyderabad, India.

出版信息

Sci Rep. 2025 May 19;15(1):17267. doi: 10.1038/s41598-025-99286-0.

Abstract

In this study, we examined the major sources of particulate organic matter (POM) in the Godavari River during high flow and low flow periods, to understand the impact of excess nitrogen (N)-fertilizers used in agricultural fields. δC of particulate organic carbon (POC) and δN of particulate nitrogen (PN), elemental carbon (C) to N ratio and POC:Chl-a ratios indicated that in-situ sources predominantly contributed (~ 60%) during low flow period, whereas, terrestrial sources largely contributed during high flow period (75-80%). This is attributed to prevailing conducive conditions such as low flow, better light availability due to low suspended matter and availability of nutrients for phytoplankton growth during former period, whereas increased transport of particulate and dissolved materials from land to river during the latter period. δN during low flow (7.4 ± 2.9‰) and high flow (9.4 ± 2.1‰) periods demonstrate that contribution of POM produced from N-fertilizers (δN: 0 ± 1‰) is not significant, rather than hitherto hypothesized. It could be due to seepage of excess N-fertilizers used in agricultural fields into groundwaters rather than transporting to rivers and/or transformation to another from through nitrification/denitrification processes within soils.

摘要

在本研究中,我们调查了戈达瓦里河在高流量和低流量时期颗粒有机物(POM)的主要来源,以了解农田中过量使用氮肥的影响。颗粒有机碳(POC)的δC和颗粒氮(PN)的δN、元素碳(C)与氮的比率以及POC:Chl-a比率表明,在低流量时期,原地来源的贡献占主导(约60%),而在高流量时期,陆地来源的贡献较大(75 - 80%)。这归因于当时的有利条件,如低流量时期水流缓慢、悬浮物少使得光照条件更好以及浮游植物生长所需养分充足,而在高流量时期,从陆地到河流的颗粒和溶解物质的输送增加。低流量(7.4±2.9‰)和高流量(9.4±2.1‰)时期的δN表明,氮肥产生的POM(δN:0±1‰)的贡献并不显著,并非如之前所假设的那样。这可能是由于农田中过量使用的氮肥渗入地下水,而非输送到河流和/或通过土壤中的硝化/反硝化过程转化为其他物质。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/d3d6/12086238/287e8b70fdbc/41598_2025_99286_Fig1_HTML.jpg

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