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长期施加氮磷钾添加对泥炭藓氮素状况的交互影响

Long-term interactive effects of N addition with P and K availability on N status of Sphagnum.

机构信息

Kyushu University Forest, Kyushu University, 394 Tsubakuro, Sasaguri, Fukuoka, 811-2415, Japan.

Centre for Ecology & Hydrology (CEH) Edinburgh, Bush Estate, Penicuik, EH26 0QB, UK.

出版信息

Environ Pollut. 2018 Jun;237:468-472. doi: 10.1016/j.envpol.2018.02.076. Epub 2018 Mar 15.

Abstract

Little information exists concerning the long-term interactive effect of nitrogen (N) addition with phosphorus (P) and potassium (K) on Sphagnum N status. This study was conducted as part of a long-term N manipulation on Whim bog in south Scotland to evaluate the long-term alleviation effects of phosphorus (P) and potassium (K) on N saturation of Sphagnum (S. capillifolium). On this ombrotrophic peatland, where ambient deposition was 8 kg N ha yr, 56 kg N ha yr of either ammonium (NH, N) or nitrate (NO, N) with and without P and K, were added over 11 years. Nutrient concentrations of Sphagnum stem and capitulum, and pore water quality of the Sphagnum layer were assessed. The N-saturated Sphagnum caused by long-term (11 years) and high doses (56 kg N ha yr) of reduced N was not completely ameliorated by P and K addition; N concentrations in Sphagnum capitula for N 56 PK were comparable with those for N 56, although N concentrations in Sphagnum stems for N 56 PK were lower than those for N 56. While dissolved inorganic nitrogen (DIN) concentrations in pore water for N 56 PK were not different from N 56, they were lower for N 56 PK than for N 56 whose stage of N saturation had not advanced compared to N 56. These results indicate that increasing P and K availability has only a limited amelioration effect on the N assimilation of Sphagnum at an advanced stage of N saturation. This study concluded that over the long-term P and K additions will not offset the N saturation of Sphagnum.

摘要

关于氮 (N) 与磷 (P) 和钾 (K) 的长期相互作用对泥炭藓 N 状态的影响,相关信息很少。本研究是在苏格兰南部 Whim 泥沼进行的一项长期 N 处理的一部分,目的是评估 P 和 K 的长期添加对 N 饱和泥炭藓(Sphagnum capillifolium)的缓解作用。在这个富营养泥炭地,环境沉积量为 8 kg N ha yr,11 年内分别添加了 56 kg N ha yr 的铵(NH,N)或硝酸盐(NO,N),并同时添加和不添加 P 和 K。评估了泥炭藓茎和帽状体的养分浓度以及泥炭藓层的孔隙水质量。长期(11 年)和高剂量(56 kg N ha yr)还原 N 导致的 N 饱和泥炭藓,通过添加 P 和 K 并未得到完全缓解;N 56 PK 处理的泥炭藓帽状体的 N 浓度与 N 56 处理的相当,尽管 N 56 PK 处理的泥炭藓茎的 N 浓度低于 N 56 处理的。虽然 N 56 PK 处理的孔隙水中的溶解无机氮(DIN)浓度与 N 56 处理的没有差异,但与未进一步进入 N 饱和阶段的 N 56 处理相比,N 56 PK 处理的 DIN 浓度较低。这些结果表明,增加 P 和 K 的有效性对 N 饱和阶段晚期泥炭藓的 N 同化只有有限的缓解作用。本研究得出的结论是,长期添加 P 和 K 不会抵消泥炭藓的 N 饱和。

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